Specifics of the Near-Surface Turbulence

Amiro BD (1990) Comparison of turbulence statistics within three boreal forest canopies. Boundary-Layer Meteorol 51:99–121. https://doi.org/10.1007/BF00120463CrossRef

Amiro BD (1998) Footprint climatologies for evapotranspiration in a boreal catchment. Agric For Meteorol 90:195–201. https://doi.org/10.1016/S0168-1923(97)00096-8CrossRef

Andreas EL, Cash BA (1999) Convective heat transfer over wintertime leads and polynyas. J Geophys Res 104(C11):25721–25734. https://doi.org/10.1029/1999JC900241CrossRef

Antonia RA, Luxton RE (1971) The response of turbulent boundary layer to a step change in surface roughness, Part 1. J Fluid Mech 48:721–761. https://doi.org/10.1017/S0022112071001824CrossRef

Antonia RA, Luxton RE (1972) The response of turbulent boundary layer to a step change in surface roughness, Part 2. J Fluid Mech 53:737–757. https://doi.org/10.1017/S002211207200045XCrossRef

Arriga N, Rannik Ü, Aubinet M, Carrara A, Vesala T, Papale D (2017) Experimental validation of footprint models for eddy covariance CO2 flux measurements above grassland by means of natural and artificial tracers. Agric For Meteorol 242:75–84. https://doi.org/10.1016/j.agrformet.2017.04.006CrossRef

Arya SP (2001) Introduction to micrometeorology. Academic, San Diego

Aubinet M (2008) Eddy covariance CO₂ flux measurements in nocturnal conditions: an analysis of the problem. Ecol Appl 18:1368–1378. https://doi.org/10.1023/A:1000472717236CrossRef

Aubinet M, Grelle A, Ibrom A, Rannik Ü, Moncrieff J, Foken T, Kowalski AS, Martin PH, Berbigier P, Bernhofer C, Clement R, Elbers J, Granier A, Grünwald T, Morgenstern K, Pilegaard K, Rebmann C, Snijders W, Valentini R, Vesala T (1999) Estimates of the annual net carbon and water exchange of forests: The EUROFLUX methodology. Adv Ecol Res 30:113–175. https://doi.org/10.1016/S0065-2504(08)60018-5CrossRef

Aubinet M, Clement R, Elbers J, Foken T, Grelle A, Ibrom A, Moncrieff H, Pilegaard K, Rannik U, Rebmann C (2003a) Methodology for data acquisition, storage and treatment. In: Valentini R (ed) Fluxes of carbon, water and energy of European Forests. Ecological Studies, vol 163. Springer, Berlin, Heidelberg, pp 9–35. https://doi.org/10.1007/978-3-662-05171-9_2CrossRef

Aubinet M, Heinesch B, Yernaux M (2003b) Horizontal and vertical CO₂ advection in a sloping forest. Boundary-Layer Meteorol 108:397–417. https://doi.org/10.1023/A:1024168428135CrossRef

Bailey WG, Oke TR, Rouse WR (eds) (1997) The surface climate of Canada. Mc Gill-Queen’s University Press, Montreal, Kingston

Baldocchi D (1997) Flux footprints within and over forest canopies. Boundary-Layer Meteorol 85:273–292. https://doi.org/10.1023/A:1000472717236CrossRef

Baldocchi DD, Finnigan J, Wilson K, Paw UKT, Falge E (2000) On measuring net ecosystem carbon exchange over tall vegetation on complex terrain. Boundary-Layer Meteorol 96:257–291. https://doi.org/10.1023/A:1002497616547CrossRef

Basu S, Holtslag AAM (2021) Turbulent Prandtl number and characteristic length scales in stably stratified flows: steady-state analytical solutions. Environ Fluid Mech 21:1273–1302. https://doi.org/10.1007/s10652-021-09820-7CrossRef

Baumgartner A (1956) Untersuchungen über den Wärme- und Wasserhaushalt eines jungen Waldes. Ber Dt Wetterdienstes 28:53

Bekkers CCA, Angelou N, Dellwik E (2022) Drag coefficient and frontal area of a solitary mature tree. J Wind Eng Ind Aerodyn 220:104854. https://doi.org/10.1016/j.jweia.2021.104854CrossRef

Belcher SE, Finnigan JJ, Harman IN (2008) Flows through forest canopies in complex terrain. Ecol Appl 18:1436–1453CrossRef

Bergström H, Högström U (1989) Turbulent exchange above a pine forest. II Organized structures. Boundary-Layer Meteorol 49:231–263. https://doi.org/10.1007/BF00120972CrossRef

Beyrich F, Mengelkamp H-T (2006) Evaporation over a heterogeneous land surface: EVA_GRIPS and the LITFASS-2003 experiment – an overview. Boundary-Layer Meteorol 121:5–32. https://doi.org/10.1007/s10546-006-9079-zCrossRef

Biermann T, Babel W, Ma W, Chen X, Thiem E, Ma Y, Foken T (2014) Turbulent flux observations and modelling over a shallow lake and a wet grassland in the Nam Co basin, Tibetan Plateau. Theor Appl Climat 116:301–316. https://doi.org/10.1007/s00704-013-0953-6CrossRef

Blay-Carreras E, Pardyjak ER, Pino D, Alexander DC, Lohou F, Lothon M (2014) Countergradient heat flux observations during the evening transition period. Atmos Chem Phys 14:9077–9085. https://doi.org/10.5194/acp-14-9077-2014CrossRef

Blay-Carreras E, Pardyjak ER, Pino D, Hoch SW, Cuxart J, Martínez D, Reuder J (2015) Lifted temperature minimum during the atmospheric evening transition. Atmos Chem Phys 15:6981–6991. https://doi.org/10.5194/acp-15-6981-2015CrossRef

Bou-Zeid E, Meneveau C, Parlange MB (2004) Large-eddy simulation of neutral atmospheric boundary layer flow over heterogeneous surfaces: blending height and effective surface roughness. Water Resources Res 40:W02505. https://doi.org/10.1029/2003WR002475

Bradley EF (1968) A micrometeorological study of velocity profiles and surface drag in the region modified by change in surface roughness. Quart J R Meteorol Soc 94:361–379. https://doi.org/10.1002/qj.49709440111CrossRef

de Bruin HAR, Moore JC (1985) Zero-plane displacement and roughness length for tall vegetation, derived from a simple mass conservation hypothesis. Boundary-Layer Meteorol 38:39–49. https://doi.org/10.1007/BF00120033CrossRef

de Bruin HAR, Bink NJ, Kroon LJ (1991) Fluxes in the surface layer under advective conditions. In: Schmugge TJ, André JC (eds) Workshop on land surface evaporation, measurement and parameterization. Springer, New York, pp 157–169CrossRef

Brunet Y, Finnigan JJ, Raupach MR (1994) A wind tunnel study of air flow in waving wheat: single-point velocity statistics. Boundary-Layer Meteorol 70:95–132. https://doi.org/10.1007/BF00712525CrossRef

Businger JA, Oncley SP (1990) Flux measurement with conditional sampling. J Atm Oceanic Techn 7:349–352. https://doi.org/10.1175/1520-0426(1990)007<0349:FMWCS>2.0.CO;2CrossRef

Cai X, Leclerc MY (2007) Forward-in-time and backward-in-time dispersion in the convective boundary layer: the concentration footprint. Boundary-Layer Meteorol 123:201–218. https://doi.org/10.1007/s10546-006-9141-xCrossRef

Campbell GS, Norman JM (2013) An introduction to environmental biophysics, 2nd edn. Springer, New York

Cellier P, Brunet Y (1992) Flux-gradient relationships above tall plant canopies. Agric For Meteorol 58:93–117. https://doi.org/10.1016/0168-1923(92)90113-ICrossRef

Charuchittipan D, Babel W, Mauder M, Leps J-P, Foken T (2014) Extension of the averaging time of the eddy-covariance measurement and its effect on the energy balance closure. Boundary-Layer Meteorol 152:303–327. https://doi.org/10.1007/s10546-014-9922-6CrossRef

Chen JM, Leblanc SG, Cihlar J, Desjardins RL, MacPherson IJ (1999) Extending aircraft- and tower-based CO₂ flux measurements to a boreal region using a Landsat thematic mapper land cover map. J Geophys Res 104(D14):16859–16877. https://doi.org/10.1029/1999JD900129CrossRef

Chu H, Luo X, Ouyang Z, Chan WS, Dengel S, Biraud SC, Torn MS, Metzger S, Kumar J, Arain MA, Arkebauer TJ, Baldocchi D, Bernacchi C, Billesbach D, Black TA, Blanken PD, Bohrer G, Bracho R, Brown S, Brunsell NA, Chen J, Chen X, Clark K, Desai AR, Duman T, Durden D, Fares S, Forbrich I, Gamon JA, Gough CM, Griffis T, Helbig M, Hollinger D, Humphreys E, Ikawa H, Iwata H, Ju Y, Knowles JF, Knox SH, Kobayashi H, Kolb T, Law B, Lee X, Litvak M, Liu H, Munger JW, Noormets A, Novick K, Oberbauer SF, Oechel W, Oikawa P, Papuga SA, Pendall E, Prajapati P, Prueger J, Quinton WL, Richardson AD, Russell ES, Scott RL, Starr G, Staebler R, Stoy PC, Stuart-Haëntjens E, Sonnentag O, Sullivan RC, Suyker A, Ueyama M, Vargas R, Wood JD, Zona D (2021) Representativeness of Eddy-Covariance flux footprints for areas surrounding AmeriFlux sites. Agric For Meteorol 301–302:108350. https://doi.org/10.1016/j.agrformet.2021.108350CrossRef

Chundshua GG, Andreev EG (1980) O mechanizme formirovanija inversii temperatury v privodnoim sloe atmosfery nad morem (About a mechanism of the developement of a temperature inversion in the near surface layer above the ocean). Dokl AN SSSR 255:829–832

Cionco RM (1978) Analysis of canopy index values for various canopy densities. Boundary-Layer Meteorol 15:81–93. https://doi.org/10.1007/BF00165507CrossRef

Claussen M (1991) Estimation of areally-averaged surface fluxes. Boundary-Layer Meteorol 54:387–410. https://doi.org/10.1007/BF00118868CrossRef

Claussen M (1995) Flux aggregation at large scales: on the limits of validity of the concept of blending height. J Hydrol 166:371–382. https://doi.org/10.1016/0022-1694(94)05098-ICrossRef

Claussen M, Walmsley JL (1994) Modification of blending procedure in a proposed new PBL resistance law. Boundary-Layer Meteorol 68:201–205. https://doi.org/10.1007/BF00712672CrossRef

Collineau S, Brunet Y (1993a) Detection of turbulent coherent motions in a forest canopy. Part I: Wavelet analysis. Boundary-Layer Meteorol 65:357–379. https://doi.org/10.1007/BF00707033CrossRef

Collineau S, Brunet Y (1993b) Detection of turbulent coherent motions in a forest canopy. Part II: Time-scales and conditional averages. Boundary-Layer Meteorol 66:49–73. https://doi.org/10.1007/BF00705459CrossRef

Culf AD, Foken T, Gash JHC (2004) The energy balance closure problem. In: Kabat P, Claussen M, Dirmeyer PA et al (eds) Vegetation, water, humans and the climate. A new perspective on an interactive system. Springer, Berlin, Heidelberg, pp 159–166. https://doi.org/10.1007/978-3-642-18948-7_13CrossRef

De Roo F, Zhang S, Huq S, Mauder M (2018) A semi-empirical model of the energy balance closure in the surface layer. PLoS One 13:e0209022. https://doi.org/10.1371/journal.pone.0209022CrossRef

Deardorff JW (1966) The counter-gradient heat flux in the lower atmosphere and in the laboratory. J Atmos Sci 23:503–506. https://doi.org/10.1175/1520-0469(1966)023<0503:tcghfi>2.0.co;2CrossRef

Denmead DT, Bradley EF (1985) Flux-gradient relationships in a forest canopy. In: Hutchison BA, Hicks BB (eds) The forest-atmosphere interaction. D. Reidel Publ. Comp., Dordrecht, Boston, London, pp 421–442. https://doi.org/10.1007/978-94-009-5305-5_27CrossRef

Denmead DT, Bradley EF (1987) On scalar transport in plant canopies. Irrig Sci 8:131–149. https://doi.org/10.1007/BF00259477CrossRef

Duarte H, Leclerc M, Zhang G, Durden D, Kurzeja R, Parker M, Werth D (2015) Impact of nocturnal low-level jets on near-surface turbulence kinetic energy. Boundary-Layer Meteorol 156:349–370. https://doi.org/10.1007/s10546-015-0030-zCrossRef

Dupont S, Brunet Y (2009) Coherent structures in canopy edge flow: a large-eddy simulation study. J Fluid Mech 630:93–128. https://doi.org/10.1017/S0022112009006739CrossRef

Eder F, Serafimovich A, Foken T (2013) Coherent structures at a forest edge: properties, coupling and impact of secondary circulations. Boundary-Layer Meteorol 148:285–308. https://doi.org/10.1007/s10546-013-9815-0CrossRef

Eigenmann R, Metzger S, Foken T (2009) Generation of free convection due to changes in the local circulation system. Atmos Chem Phys 9: 8587-8600. https://doi.org/10.5194/acp-9-8587-2009CrossRef

Elith J, Leathwick JR, Hastie T (2008) A working guide to boosted regression trees. J Animal Ecol 77:802–813. https://doi.org/10.1111/j.1365-2656.2008.01390.xCrossRef

Elliott WP (1958) The growth of the atmospheric internal boundary layer. Trans Am Geophys Union 39:1048–1054. https://doi.org/10.1029/TR039i006p01048CrossRef

Farge M (1992) Wavelet transforms and their application to turbulence. Annu Rev Fluid Mech 24:395–347. https://doi.org/10.1146/annurev.fl.24.010192.002143CrossRef

Fiedler F, Panofsky HA (1972) The geostrophic drag coefficient and the ‘effective’ roughness length. Quart J R Meteorol Soc 98:213–220. https://doi.org/10.1002/qj.49709841519CrossRef

Finn D, Lamb B, Leclerc MY, Horst TW (1996) Experimental evaluation of analytical and Lagrangian surface-layer flux footprint models. Boundary-Layer Meteorol 80:283–308. https://doi.org/10.1007/BF00119546CrossRef

Finn D, Lamb B, Leclerc MY, Lovejoy S, Pecknold S, Schertzer D (2001) Multifractal analysis of line-source plume concentration fluctuations in surface-layer flows. J Appl Meteorol 40:229–245. https://doi.org/10.1175/1520-0450(2001)040<0229:MAOLSP>2.0.CO;2CrossRef

Finnigan J (1999) A comment on the paper by Lee (1998): “On micrometeorological observations of surface-air exchange over tall vegetation'”. Agric For Meteorol 97:55–64. https://doi.org/10.1016/S0168-1923(99)00049-0CrossRef

Finnigan J (2000) Turbulence in plant canopies. Ann Rev Fluid Mech 32:519–571. https://doi.org/10.1146/annurev.fluid.32.1.519CrossRef

Finnigan J (2006) The storage term in eddy flux calculations. Agric For Meteorol 136:108–113. https://doi.org/10.1016/j.agrformet.2004.12.010CrossRef

Finnigan JJ, Clement R, Malhi Y, Leuning R, Cleugh HA (2003) A re-evaluation of long-term flux measurement techniques, Part I: Averaging and coordinate rotation. Boundary-Layer Meteorol 107:1–48. https://doi.org/10.1023/A:1021554900225CrossRef

Finnigan JJ, Shaw RH, Patton EG (2009) Turbulence structure above a vegetation canopy. J Fluid Mech 637:687–424. https://doi.org/10.1017/S0022112009990589CrossRef

Florens E, Eiff O, Moulin F (2013) Defining the roughness sublayer and its turbulence statistics. Exp Fluids 54:1500. https://doi.org/10.1007/s00348-013-1500-zCrossRef

Foken T (1990) Turbulenter Energieaustausch zwischen Atmosphäre und Unterlage – Methoden, meßtechnische Realisierung sowie ihre Grenzen und Anwendungsmöglichkeiten. Ber Dt Wetterdienstes 180:287

Foken T (1998) Die scheinbar ungeschlossene Energiebilanz am Erdboden – eine Herausforderung an die Experimentelle Meteorologie. Sitzungsberichte der Leibniz-Sozietät 24:131–150

Foken T (2008) The energy balance closure problem – An overview. Ecol Appl 18:1351–1367. https://doi.org/10.1890/06-0922.1CrossRef

Foken T (2013) Application of footprint models for wind turbine locations. Meteorol Z 22:111–115. https://doi.org/10.1127/0941-2948/2012/0390CrossRef

Foken T (2023) Decoupling between the atmosphere and the underlying surface uuring stable stratification. Boundary-Layer Meteorol 187:117–140. https://doi.org/10.1007/s10546-022-00746-1CrossRef

Foken T, Kuznecov OA (1978) Die wichtigsten Ergebnisse der gemeinsamen Expedition “KASPEX-76” des Institutes für Ozeanologie Moskau und der Karl-Marx-Universität Leipzig. Beitr Meeresforsch 41:41–47

Foken T, Leclerc MY (2004) Methods and limitations in validation of footprint models. Agric For Meteorol 127:223–234. https://doi.org/10.1016/j.agrformet.2004.07.015CrossRef

Foken T, Oncley SP (1995) Results of the workshop ‘Instrumental and methodical problems of land surface flux measurements’. Bull Amer Meteorol Soc 76:1191–1193. https://doi.org/10.1175/1520-0477-76.7.1191CrossRef

Foken T, Wichura B (1996) Tools for quality assessment of surface-based flux measurements. Agric For Meteorol 78:83–105. https://doi.org/10.1016/0168-1923(95)02248-1CrossRef

Foken T, Wimmer F, Mauder M, Thomas C, Liebethal C (2006) Some aspects of the energy balance closure problem. Atmos Chem Phys 6:4395–4402. https://doi.org/10.5194/acp-6-4395-2006CrossRef

Foken T, Mauder M, Liebethal C, Wimmer F, Beyrich F, Leps J-P, Raasch S, DeBruin HAR, Meijninger WML, Bange J (2010) Energy balance closure for the LITFASS-2003 experiment. Theor Appl Climat 101:149–160. https://doi.org/10.1007/s00704-009-0216-8CrossRef

Foken T, Aubinet M, Finnigan J, Leclerc MY, Mauder M, Paw UKT (2011) Results of a panel discussion about the energy balance closure correction for trace gases. Bull Am Meteorol Soc 92:ES13–ES18. https://doi.org/10.1175/2011BAMS3130.1

Foken T, Meixner FX, Falge E, Zetzsch C, Serafimovich A, Bargsten A, Behrendt T, Biermann T, Breuninger C, Dix S, Gerken T, Hunner M, Lehmann-Pape L, Hens K, Jocher G, Kesselmeier J, Lüers J, Mayer JC, Moravek A, Plake D, Riederer M, Rütz F, Scheibe M, Siebicke L, Sörgel M, Staudt K, Trebs I, Tsokankunku A, Welling M, Wolff V, Zhu Z (2012) Coupling processes and exchange of energy and reactive and non-reactive trace gases at a forest site – results of the EGER experiment. Atmos Chem Phys 12:1923–1950. https://doi.org/10.5194/acp-12-1923-2012CrossRef

Foken T, Serafimovich A, Eder F, Hübner J, Gao Z, Liu H (2017) Interaction forest–clearing. In: Foken T (ed) Energy and matter fluxes of a spruce forest ecosystem, Ecological studies, vol 229. Springer, Cham, pp 309–329. https://doi.org/10.1007/978-3-319-49389-3_13CrossRef

Friedrich K, Mölders N, Tetzlaff G (2000) On the influence of surface heterogeneity on the Bowen-ratio: a theoretical case study. Theor Appl Climat 65:181–196. https://doi.org/10.1007/s007040070043CrossRef

Gamage N, Hagelberg C (1993) Detection and analysis of microfronts and associated coherent events using localized transforms. J Atmos Sci 50:750–756. https://doi.org/10.1175/1520-0469(1993)050<0750:DAAOMA>2.0.CO;2CrossRef

Gao W, Shaw RH, PawU KT (1989) Observation of organized structure in turbulent flow within and above a forest canopy. Boundary-Layer Meteorol 47:349–377. https://doi.org/10.1007/BF00122339CrossRef

Garratt JR (1978) Flux profile relations above tall vegetation. Quart J R Meteorol Soc 104:199–211. https://doi.org/10.1002/qj.49710443915CrossRef

Garratt JR (1980) Surface influence upon vertical profiles in the atmospheric near surface layer. Quart J R Meteorol Soc 106:803–819. https://doi.org/10.1002/qj.49710645011CrossRef

Garratt JR (1990) The internal boundary layer – a review. Boundary-Layer Meteorol 50:171–203. https://doi.org/10.1007/BF00120524CrossRef

Garratt JR (1992) The atmospheric Boundary Layer. Cambridge University Press, Cambridge

Gash JHC (1986) A note on estimating the effect of a limited fetch on micrometeorological evaporation measurements. Boundary-Layer Meteorol 35:409–414. https://doi.org/10.1007/BF00118567CrossRef

Gatzsche K, Babel W, Falge E, Pyles RD, Paw UKT, Raabe A, Foken T (2018) Footprint-weighted tile approach for a spruce forest and a nearby patchy clearing using the ACASA model. Biogeosciences 15:2945–2960. https://doi.org/10.5194/bg-15-2945-2018CrossRef

Göckede M, Rebmann C, Foken T (2004) A combination of quality assessment tools for eddy covariance measurements with footprint modelling for the characterisation of complex sites. Agric For Meteorol 127:175–188. https://doi.org/10.1016/j.agrformet.2004.07.012CrossRef

Göckede M, Markkanen T, Mauder M, Arnold K, Leps JP, Foken T (2005) Validation of footprint models using natural tracer measurements from a field experiment. Agric For Meteorol 135:314–325. https://doi.org/10.1016/j.agrformet.2005.12.008CrossRef

Göckede M, Markkanen T, Hasager CB, Foken T (2006) Update of a footprint-based approach for the characterisation of complex measuring sites. Boundary-Layer Meteorol 118:635–655. https://doi.org/10.1007/s10546-005-6435-3CrossRef

Göckede M, Thomas C, Markkanen T, Mauder M, Ruppert J, Foken T (2007) Sensitivity of Lagrangian stochastic footprints to turbulence statistics. Tellus 59B:577–586. https://doi.org/10.1111/j.1600-0889.2007.00275.xCrossRef

Göckede M, Foken T, Aubinet M, Aurela M, Banza J, Bernhofer C, Bonnefond J-M, Brunet Y, Carrara A, Clement R, Dellwik E, Elbers JA, Eugster W, Fuhrer J, Granier A, Grünwald T, Heinesch B, Janssens IA, Knohl A, Koeble R, Laurila T, Longdoz B, Manca G, Marek M, Markkanen T, Mateus J, Matteucci G, Mauder M, Migliavacca M, Minerbi S, Moncrieff JB, Montagnani L, Moors E, Ourcival J-M, Papale D, Pereira J, Pilegaard K, Pita G, Rambal S, Rebmann C, Rodrigues A, Rotenberg E, Sanz MJ, Sedlak P, Seufert G, Siebicke L, Soussana JF, Valentini R, Vesala T, Verbeeck H, Yakir D (2008) Quality control of CarboEurope flux data – Part 1: Coupling footprint analyses with flux data quality assessment to evaluate sites in forest ecosystems. Biogeosciences 5:433–450. https://doi.org/10.5194/bg-5-433-2008CrossRef

Gosselin FP (2019) Mechanics of a plant in fluid flow. J Exp Bot 70:3533–3548. https://doi.org/10.1093/jxb/erz288CrossRef

Goudriaan J (1977) Crop micrometeorology: a simulation study. In Center for Agricultural Publishing and Documentation, Wageningen, S 249

Grachev AA, Andreas EL, Fairall CW, Guest PS, Persson POG (2007) On the turbulent Prandtl number in the stable atmospheric boundary layer. Boundary-Layer Meteorol 125:329–341. https://doi.org/10.1007/s10546-007-9192-7CrossRef

Grachev AA, Andreas EL, Fairall CW, Guest PS, Persson POG (2012) Outlier problem in evaluating similarity functions in the stable atmospheric Boundary Layer. Boundary-Layer Meteorol 144:137–155. https://doi.org/10.1007/s10546-012-9714-9CrossRef

Grachev AA, Leo LS, Fernando HJS, Fairall CW, Creegan E, Blomquist BW, Christman AJ, Hocut CM (2018) Air–Sea/Land interaction in the coastal zone. Boundary-Layer Meteorol 167:181–210. https://doi.org/10.1007/s10546-017-0326-2CrossRef

Graefe J (2004) Roughness layer corrections with emphasis on SVAT model applications. Agric For Meteorol 124:237–251. https://doi.org/10.1016/j.agrformet.2004.01.003CrossRef

Grimmond CSB, Oke TR (1999) Aerodynamic properties of urban areas derived from analysis of surface form. J Appl Meteorol 38:1262–1292. https://doi.org/10.1175/1520-0450(1999)038<1262:APOUAD>2.0.CO;2CrossRef

Grimmond CSB, Oke TR (2000) Corrigendum. J Appl Meteorol 39:2494. https://doi.org/10.1175/1520-0450(2000)039<2494:C>2.0.CO;2CrossRef

Gryning S-E, van Ulden AP, Larsen S (1983) Dispersions from a ground level source investigated by a K model. Quart J R Meteorol Soc 109:355–364. https://doi.org/10.1002/qj.49710946008CrossRef

Halberstam I, Schieldge JP (1981) Anomalous behavior of the atmospheric surface layer over a melting snowpack. J Appl Meteorol Climatol 20:255–265. https://doi.org/10.1175/1520-0450(1981)020<0255:ABOTAS>2.0.CO;2CrossRef

Handorf D, Foken T (1997) Analysis of turbulent structure over an Antarctic ice shelf by means of wavelet transformation. In: 12th Symosium on boundary layer and turbulence, Vancouver BC, Canada, 28 July – 1 August 1997. Am Meteorol Soc, S 245–246

Hari P, Heliövaara K, Kulmala L (eds) (2013) Physical and physiological forest ecology. Springer, Dordrecht, Heidelberg, New York, London. https://doi.org/10.1007/978-94-007-5603-8CrossRef

Harman I (2011) The role of roughness sublayer dynamics within surface exchange schemes. Boundary-Layer Meteorol, 1–20. https://doi.org/10.1007/s10546-011-9651-z

Harman IN, Finnigan JJ (2007) A simple unified theory for flow in the canopy and roughness sublayer. Boundary-Layer Meteorol 123:339–363. https://doi.org/10.1007/s10546-006-9145-6CrossRef

Harman IN, Finnigan JJ (2008) Scalar concentration profiles in the canopy and roughness sublayer. Boundary-Layer Meteorol 129:323–351. https://doi.org/10.1007/s10546-008-9328-4CrossRef

Hasager CB, Jensen NO (1999) Surface-flux aggregation in heterogeneous terrain. Quart J R Meteorol Soc 125:2075–2102. https://doi.org/10.1002/qj.49712555808CrossRef

Haverd V, Cuntz M, Leuning R, Keith H (2007) Air and biomass heat storage fluxes in a forest canopy: calculation within a soil vegetation atmosphere transfer model. Agric For Meteorol 147:125–139. https://doi.org/10.1016/j.agrformet.2007.07.006CrossRef

Heidbach K, Schmid HP, Mauder M (2017) Experimental evaluation of flux footprint models. Agric For Meteorol 246:142–153. https://doi.org/10.1016/j.agrformet.2017.06.008CrossRef

Heusinkveld BG, Jacobs AFG, Holtslag AAM, Berkowicz SM (2004) Surface energy balance closure in an arid region: role of soil heat flux. Agric For Meteorol 122:21–37. https://doi.org/10.1016/j.agrformet.2003.09.005CrossRef

Holmes P, Lumley JL, Berkooz G (1996) Turbulence, coherent structures, dynamical systems and symmetry. Cambridge University Press, CambridgeCrossRef

Holtslag AAM, Nieuwstadt FTM (1986) Scaling the atmospheric boundary layer. Boundary-Layer Meteorol 36:201–209. https://doi.org/10.1007/BF00117468CrossRef

Horst TW (1999) The footprint for estimation of atmosphere-surface exchange fluxes by profile techniques. Boundary-Layer Meteorol 90:171–188. https://doi.org/10.1023/A:1001774726067CrossRef

Horst TW, Weil JC (1992) Footprint estimation for scalar flux measurements in the atmospheric surface layer. Boundary-Layer Meteorol 59:279–296. https://doi.org/10.1007/BF00119817CrossRef

Horst TW, Weil JC (1994) How far is far enough?: The fetch requirements for micrometeorological measurement of surface fluxes. J Atm Oceanic Techn 11:1018–1025. https://doi.org/10.1175/1520-0426(1994)011<1018:HFIFET>2.0.CO;2CrossRef

Horst TW, Weil JC (1995) Corrigendum J Atm Oceanic Techn 12:447. https://doi.org/10.1175/1520-0426(1995)012<0447:>2.0.CO;2CrossRef

Hsieh C-I, Katul G (2009) The Lagrangian stochastic model for estimating footprint and water vapor fluxes over inhomogeneous surfaces. Int J Biometeorol 53:87–100. https://doi.org/10.1007/s00484-008-0193-0CrossRef

Hsieh C-I, Katul G, Chi T-W (2000) An approximate analytical model for footprint estimation of scalar fluxes in thermally stratified atmospheric flows. Adv Water Res 23:765–772. https://doi.org/10.1016/S0309-1708(99)00042-1CrossRef

Huang J, Lee X, Patton EG (2008) A modelling study of flux imbalance and the influence of entrainment in the convective Boundary Layer. Boundary-Layer Meteorol 127:273–292. https://doi.org/10.1007/s10546-007-9254-xCrossRef

Hupfer P, Foken T, Bachstein U (1976) Fine structure of the internal boundary layer in the near shore zone of the sea. Boundary-Layer Meteorol 10:503–505. https://doi.org/10.1007/BF00225868CrossRef

Hurtalová T, Matejka F, Vidovic J (1983) Untersuchung der Oberflächenrauhigkeit und ihrer Variation auf Grund von Strukturveränderungen des Maisbestandes während der Ontogenese. Z Meteorol 33:368–372

Hurtalova T, Vidovitsch J, Matejka F, Mudry P (1988) Dinamitscheskaja sherochovatost i biometritscheskie charakteristiki kukuruzy v ontogeneze (Dynamical roughness and biometric characteristics of corn during the ontogenesis). Contr Geophys Inst Slovak Akad Sci 8:46–53

Hutjes RWA, Vellinga OS, Gioli B, Miglietta F (2010) Dis-aggregation of airborne flux measurements using footprint analysis. Agric For Meteorol 150:966–983. https://doi.org/10.1016/j.agrformet.2010.03.004CrossRef

Inclán MG, Forkel R, Dlugi R, Stull RB (1996) Application of transilient turbulent theory to study interactions between the atmospheric boundary layer and forest canopies. Boundary-Layer Meteorol 79:315–344. https://doi.org/10.1007/BF00119403CrossRef

Ingwersen J, Steffens K, Högy P, Warrach-Sagi K, Zhunusbayeva D, Poltoradnev M, Gäbler R, Wizemann H-D, Fangmeier A, Wulfmeyer V, Streck T (2011) Comparison of Noah simulations with eddy covariance and soil water measurements at a winter wheat stand. Agric For Meteorol 151:345–355. https://doi.org/10.1016/j.agrformet.2010.11.010CrossRef

Jegede OO, Foken T (1999) A study of the internal boundary layer due to a roughness change in neutral conditions observed during the LINEX field campaigns. Theor Appl Climat 62:31–41. https://doi.org/10.1007/s007040050072CrossRef

Jocher G, Ottosson Löfvenius M, De Simon G, Hörnlund T, Linder S, Lundmark T, Marshall J, Nilsson MB, Näsholm T, Tarvainen L, Öquist M, Peichl M (2017) Apparent winter CO₂ uptake by a boreal forest due to decoupling. Agric For Meteorol 232:23–34. https://doi.org/10.1016/j.agrformet.2016.08.002CrossRef

Jones HG (2013) Plants and microclimate, 3rd edn. Cambridge Univ. Press, Cambridge. https://doi.org/10.1017/CBO9780511845727CrossRef

Kaharabata SK, Schuepp PH, Ogunjemiyo S, Shen S, Leclerc MY, Desjardins RL, MacPherson JI (1997) Footprint considerations in BOREAS. J Geophys Res 102(D24):29113–29124. https://doi.org/10.1029/97JD02559CrossRef

Kaimal JC, Finnigan JJ (1994) Atmospheric boundary layer flows: their structure and measurement. Oxford University Press, New York, NY. https://doi.org/10.1093/oso/9780195062397.001.0001CrossRef

Kanani-Sühring F, Raasch S (2015) Spatial variability of scalar concentrations and fluxes downstream of a clearing-to-forest transition: a Large-Eddy Simulation study. Boundary-Layer Meteorol 155:1–27. https://doi.org/10.1007/s10546-014-9986-3CrossRef

Kanda M, Moriwaki R, Roth M, Oke T (2002) Area-averaged sensible heat flux and a new method to determine zero-plane displacement length over an urban surface using scintillometry. Boundary-Layer Meteorol 105:177–193. https://doi.org/10.1023/A:1019668424982CrossRef

Kanda M, Inagaki A, Letzel MO, Raasch S, Watanabe T (2004) LES study of the energy imbalance problem with eddy covariance fluxes. Boundary-Layer Meteorol 110:381–404. https://doi.org/10.1023/B:BOUN.0000007225.45548.7aCrossRef

Karipot A, Leclerc MY, Zhang G, Lewin KF, Nagy J, Hendrey GR, Starr D (2008) Influence of nocturnal low-level jet on turbulence structure and CO₂ flux measurements over a forest canopy. J Geophys Res 113:D10102. https://doi.org/10.1029/2007JD009149CrossRef

Kent CW, Grimmond S, Barlow J, Gatey D, Kotthaus S, Lindberg F, Halios CH (2017) Evaluation of urban local-scale aerodynamic parameters: implications for the vertical profile of wind speed and for source areas. Boundary-Layer Meteorol 164:183–213. https://doi.org/10.1007/s10546-017-0248-zCrossRef

Kitajgorodskij SA, Volkov JA (1965) O rascete turbulentnych potokov tepla i vlagi v privodnom sloe atmosfery (The calculation of the turbulent fluxes of temperature and humidity in the atmosphere near the water surface) Izv AN SSSR. Fiz Atm i Okeana 1:1317–1336

Klaassen W, Sogatchev A (2006) Flux footprint simulation downwind of a forest edge. Boundary-Layer Meteorol 121:459–473. https://doi.org/10.1007/s10546-006-9078-0CrossRef

Klaassen W, van Breugel PB, Moors EJ, Nieveen JP (2002) Increased heat fluxes near a forest edge. Theor Appl Climat 72:231–243. https://doi.org/10.1007/s00704-002-0682-8CrossRef

Kljun N, Rotach MW, Schmid HP (2002) A three-dimensional backward Lagrangian footprint model for a wide range of boundary layer stratification. Boundary-Layer Meteorol 103:205–226. https://doi.org/10.1023/A:1014556300021CrossRef

Kljun N, Calanca P, Rotach M, Schmid HP (2004) A simple parameterization for flux footprint predictions. Boundary-Layer Meteorol 112:503–523. https://doi.org/10.1023/B:BOUN.0000030653.71031.96CrossRef

Kljun N, Calanca P, Rotach MW, Schmid HP (2015) A simple two-dimensional parameterisation for Flux Footprint Prediction (FFP). Geosci Model Dev 8(11):3695–3713. https://doi.org/10.5194/gmd-8-3695-2015CrossRef

Kohsiek W, Liebethal C, Foken T, Vogt R, Oncley SP, Bernhofer C, DeBruin HAR (2007) The energy balance experiment EBEX-2000. Part III: Behaviour and quality of radiation measurements. Boundary-Layer Meteorol 123:55–75. https://doi.org/10.1007/s10546-006-9135-8CrossRef

Koitzsch R, Dzingel M, Foken T, Mücket G (1988) Probleme der experimentellen Erfassung des Energieaustausches über Winterweizen. Z Meteorol 38:150–155

Kormann R, Meixner FX (2001) An analytical footprint model for non-neutral stratification. Boundary-Layer Meteorol 99:207–224. https://doi.org/10.1023/A:1018991015119CrossRef

Kracher D, Mengelkamp H-T, Foken T (2009) The residual of the energy balance closure and its influence on the results of three SVAT models. Meteorol Z 18:647–661. https://doi.org/10.1127/0941-2948/2009/0412CrossRef

Krapez JC, Ky GA (2023) Semi-analytical footprint model compliant with arbitrary atmospheric stratification: application to Monin–Obukhov profiles. Boundary-Layer Meteorol 187:743–791. https://doi.org/10.1007/s10546-023-00793-2CrossRef

Kukharets VP, Nalbandyan HG, Foken T (2000) Thermal interactions between the underlying surface and a nonstationary radiation flux. Izv Atmos Ocenanic Phys 36:318–325

de La Casinière AC (1974) Heat exchange over a melting snow surface. J Glaciol 13(67):55–72. https://doi.org/10.3189/S0022143000023376CrossRef

Leclerc MY, Thurtell GW (1989) Footprint predictions of scalar fluxes and concentration profiles using a markovian analysis In: 19th Conference of agricultural and forest meteorology, Charleston, SC, March 7–10, 1989. American Meteorological Society

Leclerc MY, Foken T (2014) Footprints in micrometeorology and ecology. Springer, Heidelberg, New York, Dordrecht, London. https://doi.org/10.1007/978-3-642-54545-0CrossRef

Leclerc MY, Thurtell GW (1990) Footprint prediction of scalar fluxes using a Markovian analysis. Boundary-Layer Meteorol 52:247–258. https://doi.org/10.1007/BF00122089CrossRef

Leclerc MY, Shen S, Lamb B (1997) Observations and large-eddy simulation modeling of footprints in the lower convective boundary layer. J Geophys Res 102(D8):9323–9334. https://doi.org/10.1029/96JD03984CrossRef

Lee R (1978) Forest microclimatology. Columbia University Press, New York

Lee X (1998) On micrometeorological observations of surface-air exchange over tall vegetation. Agric For Meteorol 91:39–49. https://doi.org/10.1016/S0168-1923(98)00071-9CrossRef

Lettau H (1969) Note on aerodynamic roughness-parameter estimation on the basis of roughness-element description. J Appl Meteorol 8:828–832. https://doi.org/10.1175/1520-0450(1969)008<0828:NOARPE>2.0.CO;2CrossRef

Leuning R, van Gorsel E, Massman WJ, Isaac PR (2012) Reflections on the surface energy imbalance problem. Agric For Meteorol 156:65–74. https://doi.org/10.1016/j.agrformet.2011.12.002CrossRef

Liebethal C (2006) On the determination of the ground heat flux in micrometeorology and its influence on the energy balance closure. PhD thesis, University of Bayreuth, Bayreuth

Lindroth A, Mölder M, Lagergren F (2010) Heat storage in forest biomass improves energy balance closure. Biogeosciences 7:301–313. https://doi.org/10.5194/bg-7-301-2010CrossRef

Logan E, Fichtl GH (1975) Rough to smooth transition of the equilibrium neutral constant stress layer. Boundary-Layer Meteorol 8:525–528. https://doi.org/10.1007/BF02153569CrossRef

Lothon M, Lohou F, Pino D, Couvreux F, Pardyjak ER, Reuder J, Vilà-Guerau de Arellano J, Durand P, Hartogensis O, Legain D, Augustin P, Gioli B, Lenschow DH, Faloona I, Yagüe C, Alexander DC, Angevine WM, Bargain E, Barrié J, Bazile E, Bezombes Y, Blay-Carreras E, van de Boer A, Boichard JL, Bourdon A, Butet A, Campistron B, de Coster O, Cuxart J, Dabas A, Darbieu C, Deboudt K, Delbarre H, Derrien S, Flament P, Fourmentin M, Garai A, Gibert F, Graf A, Groebner J, Guichard F, Jiménez MA, Jonassen M, van den Kroonenberg A, Magliulo V, Martin S, Martinez D, Mastrorillo L, Moene AF, Molinos F, Moulin E, Pietersen HP, Piguet B, Pique E, Román-Cascón C, Rufin-Soler C, Saïd F, Sastre-Marugán M, Seity Y, Steeneveld GJ, Toscano P, Traullé O, Tzanos D, Wacker S, Wildmann N, Zaldei A (2014) The BLLAST field experiment: Boundary-Layer late afternoon and sunset turbulence. Atmos Chem Phys 14:10931–10960. https://doi.org/10.5194/acp-14-10931-2014CrossRef

Lüers J, Bareiss J (2010) The effect of misleading surface temperature estimations on the sensible heat fluxes at a high Arctic site – the Arctic Turbulence Experiment 2006 on Svalbard (ARCTEX-2006). Atmos Chem Phys 10:157–168. https://doi.org/10.5194/acp-10-157-2010CrossRef

Mahrt L (1991) Eddy asymmetry in the sheared heated boundary layer. J Atmos Sci 48:472–492. https://doi.org/10.1175/1520-0469(1991)048<0472:EAITSH>2.0.CO;2CrossRef

Mahrt L (1996) The bulk aerodynamic formulation over heterogeneous surfaces. Boundary-Layer Meteorol 78:87–119. https://doi.org/10.1007/BF00122488CrossRef

Mahrt L, Richardson S, Seaman N, Stauffer D (2012) Turbulence in the nocturnal boundary layer with light and variable winds. Quart J R Meteorol Soc 138(667):1430–1439. https://doi.org/10.1002/qj.1884CrossRef

Mahrt L, Thomas C, Richardson S, Seaman N, Stauffer D, Zeeman M (2013) Non-stationary generation of weak turbulence for very stable and weak-wind conditions. Boundary-Layer Meteorol 147:179–199. https://doi.org/10.1007/s10546-012-9782-xCrossRef

Markkanen T, Steinfeld G, Kljun N, Raasch S, Foken T (2009) Comparison of conventional Lagrangian stochastic footprint models against LES driven footprint estimates. Atmos Chem Phys 9:5575–5586. https://doi.org/10.5194/acp-9-5575-2009CrossRef

Marunitsch SV (1971) Charakteristiki turbulentnosti v yslovijach lesa po gradientnym i strukturnym nabljudenijam (Turbulence characteristics of gradients in a forest from structure observations). Trudy Gos Gidrometeorol Inst 198:154–165

Mason PJ (1988) The formation of areally-averaged roughness length. Quart J R Meteorol Soc 114:399–420. https://doi.org/10.1002/qj.49711448007CrossRef

Mauder M, Foken T (2006) Impact of post-field data processing on eddy covariance flux estimates and energy balance closure. Meteorol Z 15:597–609. https://doi.org/10.1127/0941-2948/2006/0167CrossRef

Mauder M, Liebethal C, Göckede M, Leps J-P, Beyrich F, Foken T (2006) Processing and quality control of flux data during LITFASS-2003. Boundary-Layer Meteorol 121:67–88. https://doi.org/10.1007/s10546-006-9094-0CrossRef

Mauder M, Jegede OO, Okogbue EC, Wimmer F, Foken T (2007a) Surface energy flux measurements at a tropical site in West-Africa during the transition from dry to wet season. Theor Appl Climat 89:171–183. https://doi.org/10.1007/s00704-006-0252-6CrossRef

Mauder M, Oncley SP, Vogt R, Weidinger T, Ribeiro L, Bernhofer C, Foken T, Kohsiek W, DeBruin HAR, Liu H (2007b) The Energy Balance Experiment EBEX-2000. Part II: Intercomparison of eddy covariance sensors and post-field data processing methods. Boundary-Layer Meteorol 123:29–54. https://doi.org/10.5194/bg-5-451-2008CrossRef

Mauder M, Cuntz M, Drüe C, Graf A, Rebmann C, Schmid HP, Schmidt M, Steinbrecher R (2013) A strategy for quality and uncertainty assessment of long-term eddy-covariance measurements. Agric For Meteorol 169:122–135. https://doi.org/10.1016/j.agrformet.2012.09.006CrossRef

Mauder M, Foken T, Cuxart J (2020) Surface energy balance closure over land: a review. Boundary-Layer Meteorol 177:395–426. https://doi.org/10.1007/s10546-020-00529-6CrossRef

Mauder M, Ibrom A, Wanner L, De Roo F, Brugger P, Kiese R, Pilegaard K (2021) Options to correct local turbulent flux measurements for large-scale fluxes using an approach based on large-eddy simulation. Atmos Meas Tech 14:7835–7850. https://doi.org/10.5194/amt-14-7835-2021CrossRef

Maurer KD, Bohrer G, Kenny WT, Ivanov VY (2015) Large-eddy simulations of surface roughness parameter sensitivity to canopy-structure characteristics. Biogeosciences 12:2533–2548. https://doi.org/10.5194/bg-12-2533-2015CrossRef

Meijninger WML, Lüdi A, Beyrich F, Kohsiek W, DeBruin HAR (2006) Scintillometer-based turbulent surface fluxes of sensible and latent heat over heterogeneous a land surface – a contribution to LITFASS-2003. Boundary-Layer Meteorol 121:89–110. https://doi.org/10.1007/s10546-005-9022-8CrossRef

Metzger S (2018) Surface-atmosphere exchange in a box: making the control volume a suitable representation for in-situ observations. Agric For Meteorol 255:68–80. https://doi.org/10.1016/j.agrformet.2017.08.037CrossRef

Metzger S, Junkermann W, Mauder M, Butterbach-Bahl K, Trancón y Widemann B, Neidl F, Schäfer K, Wieneke S, Zheng XH, Schmid HP, Foken T (2013) Spatial resolution and regionalization of airborne flux measurements using environmental response functions. Biogeosciences 10:2193–2217. https://doi.org/10.5194/bg-10-2193-2013CrossRef

Meyers TP, Paw UKT (1986) Testing a higher-order closure model for modelling airflow within and above plant canopies. Boundary-Layer Meteorol 37:297–311. https://doi.org/10.1007/BF00122991CrossRef

Meyers TP, Paw UKT (1987) Modelling the plant canopy microenvironment with higher-order closure principles. Agric For Meteorol 41:143–163. https://doi.org/10.1016/0168-1923(87)90075-XCrossRef

Mölder M, Grelle A, Lindroth A, Halldin S (1999) Flux-profile relationship over a boreal forest – roughness sublayer correction. Agric For Meteorol 98-99:645–648. https://doi.org/10.1016/S0168-1923(99)00131-8CrossRef

Monson R, Baldocchi D (2014) Terrestrial biosphere-atmosphere fluxes. Cambridge University Press, New York. https://doi.org/10.1017/CBO9781139629218CrossRef

Morin TH, Bohrer G, Stefanik KC, Rey-Sanchez AC, Matheny AM, Mitsch WJ (2017) Combining eddy-covariance and chamber measurements to determine the methane budget from a small, heterogeneous urban floodplain wetland park. Agric For Meteorol 237–238:160–170. https://doi.org/10.1016/j.agrformet.2017.01.022CrossRef

Morse AP, Gardiner BA, Marshall BJ (2002) Mechanisms controlling turbulence development across a forest edge. Boundary-Layer Meteorol 103:227–251. https://doi.org/10.1023/a:1014507727784CrossRef

Nakai T, van der Molen MK, Gash JHC, Kodama Y (2006) Correction of sonic anemometer angle of attack errors. Agric For Meteorol 136:19–30. https://doi.org/10.1016/j.agrformet.2006.01.006CrossRef

Nakamura R, Mahrt L (2006) Vertically integrated sensible-heat budgets for stable nocturnal boundary layers. Quart J R Meteorol Soc 132:383–403. https://doi.org/10.1256/qj.05.50CrossRef

Nappo CJ (2012) An introduction to atmospheric gravity waves, 2nd edn. Academic, San Diego

Nikuradse J (1933) Strömungsgesetze an rauhen Rohren. VDI Forschungshefte 361

Ogunjemiyo SO, Kaharabata SK, Schuepp PH, MacPherson IJ, Desjardins RL, Roberts DA (2003) Methods of estimating CO₂, latent heat and sensible heat fluxes from estimates of land cover fractions in the flux footprint. Agric For Meteorol 117:125–144. https://doi.org/10.1016/S0168-1923(03)00061-3CrossRef

Oliveira BRF, Keizer JJ, Foken T (2022) Changes of the aerodynamic characteristics of a flux site after an extensive windthrow. Biogeosciences 19:2235–2243. https://doi.org/10.5194/bg-19-2235-2022CrossRef

Oncley SP, Foken T, Vogt R, Kohsiek W, DeBruin HAR, Bernhofer C, Christen A, van Gorsel E, Grantz D, Feigenwinter C, Lehner I, Liebethal C, Liu H, Mauder M, Pitacco A, Ribeiro L, Weidinger T (2007) The energy balance experiment EBEX-2000, Part I: Overview and energy balance. Boundary-Layer Meteorol 123:1–28. https://doi.org/10.1007/s10546-007-9161-1CrossRef

Panin G, Bernhofer C (2008) Parametrization of turbulent fluxes over inhomogeneous landscapes. Izvestiya Atmos Ocean Phys 44:701–716. https://doi.org/10.1134/s0001433808060030CrossRef

Panin GN, Tetzlaff G, Raabe A (1998) Inhomogeneity of the land surface and problems in the parameterization of surface fluxes in natural conditions. Theor Appl Climat 60:163–178. https://doi.org/10.1007/s007040050041CrossRef

Panofsky HA (1984) Vertical variation of roughness length at the Boulder Atmospheric Observatory. Boundary-Layer Meteorol 28:305–308. https://doi.org/10.1007/BF00121309CrossRef

Paw UKT, Baldocchi D, Meyers TP, Wilson KB (2000) Correction of eddy covariance measurements incorporating both advective effects and density fluxes. Boundary-Layer Meteorol 97:487–511. https://doi.org/10.1023/A:1002786702909CrossRef

Pearson RJ Jr, Oncley SP, Delany AC (1998) A scalar similarity study based on surface layer ozone measurements over cotton during the California Ozone Deposition Experiment. J Geophys Res 103(D15):18919–18926. https://doi.org/10.1029/98JD01479CrossRef

Peltola O, Lapo K, Thomas CK (2021) A physics-based universal indicator for vertical decoupling and mixing across canopies architectures and dynamic stabilities. Geophys Res Lett 48(5):e2020GL091615. https://doi.org/10.1029/2020GL091615CrossRef

Peltola O, Aurela M, Launiainen S, Katul G (2022) Probing eddy size and its effective mixing length in stably stratified roughness sublayer flows. Quart J R Meteorol Soc 148(749):3756–3773. https://doi.org/10.1002/qj.4386CrossRef

Perera MD (1981) Shelder behind two dimensional solit and porous fences. J Wind Eng Ind Aerodyn 8:93–104. https://doi.org/10.1016/0167-6105(81)90010-6CrossRef

Petersen EL, Troen I (1989) The European Wind Atlas. RISØ National Laboratory, Roskilde

Peterson EW (1969) Modification of mean flow and turbulent energy by a change in surface roughness under conditions of neutral stability. Quart J R Meteorol Soc 95:561–575. https://doi.org/10.1002/qj.49709540509CrossRef

Pfister L, Lapo K, Sayde C, Selker J, Mahrt L, Thomas CK (2019) Classifying the nocturnal atmospheric boundary layer into temperature and flow regimes. Quart J R Meteorol Soc 145(721):1515–1534. https://doi.org/10.1002/qj.3508CrossRef

Philip JR (1997) Blending and internal boundary-layer heights, and shear stress. Boundary-Layer Meteorol 84:85–89. https://doi.org/10.1023/A:1000345015838CrossRef

Prabha T, Leclerc MY, Baldocchi D (2008) Comparison of in-canopy flux footprints between Large-Eddy simulation and the Langrangian simulation. J Appl Meteorol Climatol 47:2115–2128. https://doi.org/10.1175/2008JAMC1814.1CrossRef

Pyles RD, Weare BC, Paw UKT (2000) The UCD Advanced Canopy-Atmosphere-Soil Algorithm: comparisons with observations from different climate and vegetation regimes. Quart J R Meteorol Soc 126:2951–2980. https://doi.org/10.1002/qj.49712656917CrossRef

Queck R, Bernhofer C, Bienert A, Eipper T, Goldberg V, Harmansa S, Hildebrand V, Maas H-G, Schlegel F, Stiller J (2015) TurbEFA: an interdisciplinary effort to investigate the turbulent flow across a forest clearing. Meteorol Z 23:637–659. https://doi.org/10.1127/metz/2014/0567CrossRef

Raabe A (1983) On the relation between the drag coefficient and fetch above the sea in the case of off-shore wind in the near shore zone. Z Meteorol 33:363–367

Raabe A (1991) Die Höhe der internen Grenzschicht. Z Meteorol 41:251–261

Radikevitsch VM (1971) Transformazija dinamitscheskich charakteristik vozduschnogo potoka pod vlijaniem izmenenija scherochovatosti postilajustschej poverchnosti (Transformation of the dynamical characteristics of the wind field under the influence of a changing surface roughness) Izv AN SSSR. Fiz Atm i Okeana 7:1241–1250

Rannik Ü, Aubinet M, Kurbanmuradov O, Sabelfeld KK, Markkanen T, Vesala T (2000) Footprint analysis for measurements over heterogeneous forest. Boundary-Layer Meteorol 97:137–166. https://doi.org/10.1023/A:1002702810929CrossRef

Rannik Ü, Markkanen T, Raittila T, Hari P, Vesala T (2003) Turbulence statistics inside and above forest: influence on footprint prediction. Boundary-Layer Meteorol 109:163–189. https://doi.org/10.1023/A:1025404923169CrossRef

Rannik Ü, Sogachev A, Foken T, Göckede M, Kljun N, Leclerc MY, Vesala T (2012) Footprint analysis. In: Aubinet M, Vesala T, Papale D (eds) Eddy covariance: a practical guide to measurement and data analysis. Springer, Berlin, Heidelberg, pp 211–261. https://doi.org/10.1007/978-94-007-2351-1_8CrossRef

Rao KS, Wyngaard JC, Coté OR (1974) The structure of the two-dimensional internal boundary layer over a sudden change of surface roughness. J Atmos Sci 31:738–746. https://doi.org/10.1175/1520-0469(1974)031<0738:TSOTTD>2.0.CO;2CrossRef

Raupach MR (1992) Drag and drag partition on rough surfaces. Boundary-Layer Meteorol 60:375–395. https://doi.org/10.1007/BF00155203CrossRef

Raupach MR (1994) Simplified expressions for vegetation roughness lenght and zero-plane displacement as functions of canopy height and area index. Boundary-Layer Meteorol 71:211–216. https://doi.org/10.1007/BF00709229CrossRef

Raupach MR, Legg BJ (1984) The uses and limitations of flux-gradient relationships in micrometeorology. Agricult Water Managem 8:119–131. https://doi.org/10.1016/0378-3774(84)90049-0CrossRef

Raupach MR, Thom AS, Edwards I (1980) A wind-tunnel study of turbulent flow close to regularly arrayed rough surface. Boundary-Layer Meteorol 18:373–379. https://doi.org/10.1007/BF00119495CrossRef

Raupach MR, Finnigan JJ, Brunet Y (1996) Coherent eddies and turbulence in vegetation canopies: the mixing-layer analogy. Boundary-Layer Meteorol 78:351–382. https://doi.org/10.1007/978-94-017-0944-6_15CrossRef

Raynor GS, Michael P, Brown RM, SethuRaman S (1975) Studies of atmospheric diffusion from a nearshore oceanic site. J Clim Appl Meteorol 14:1080–1094. https://doi.org/10.1175/1520-0450(1975)014<1080:SOADFA>2.0.CO;2CrossRef

Rebmann C, Göckede M, Foken T, Aubinet M, Aurela M, Berbigier P, Bernhofer C, Buchmann N, Carrara A, Cescatti A, Ceulemans R, Clement R, Elbers J, Granier A, Grünwald T, Guyon D, Havránková K, Heinesch B, Knohl A, Laurila T, Longdoz B, Marcolla B, Markkanen T, Miglietta F, Moncrieff H, Montagnani L, Moors E, Nardino M, Ourcvial J-M, Rambal S, Rannik U, Rotenberg E, Sedlak P, Unterhuber G, Vesala T, Yakir D (2005) Quality analysis applied on eddy covariance measurements at complex forest sites using footprint modelling. Theor Appl Climat 80:121–141. https://doi.org/10.1007/s00704-004-0095-yCrossRef

Reth S, Göckede M, Falge E (2005) CO₂ efflux from agricultural soils in Eastern Germany – comparison of a closed chamber system with eddy covariance measurements. Theor Appl Climat 80:105–120. https://doi.org/10.1007/s00704-004-0094-zCrossRef

Ross J (1981) The radiation regime and architecture of plant stands. Dr. W. Junk Publishers, The HagueCrossRef

Roth M, Salmond J, Satyanarayana A (2006) Methodological considerations regarding the measurement of turbulent fluxes in the urban roughness sublayer: the role of scintillometry. Boundary-Layer Meteorol 121:351–375. https://doi.org/10.1007/s10546-006-9074-4CrossRef

Rummel U, Ammann C, Meixner FX (2002) Characterizing turbulent trace gas exchange above a dense tropical rain forest using wavelet and surface renewal analysis. In: 15th Symposium on Boundary Layer and Turbulence, Wageningen, NL, 15–19 July 2002. Am Meteorol Soc, S 602–605

Ruppert J, Thomas C, Foken T (2006) Scalar similarity for relaxed eddy accumulation methods. Boundary-Layer Meteorol 120:39–63. https://doi.org/10.1007/s10546-005-9043-3CrossRef

Savelyev SA, Taylor PA (2001) Notes on an internal boundary-layer height formula. Boundary-Layer Meteorol 101:293–301. https://doi.org/10.1023/A:1019208631216CrossRef

Savelyev SA, Taylor PA (2005) Internal boundary layers: I. Height formulae for neutral and diabatic flow. Boundary-Layer Meteorol 115:1–25. https://doi.org/10.1007/s10546-004-2122-zCrossRef

Scanlon TM, Albertson JD (2001) Turbulent transport of carbon dioxide and water vapor within a vegetation canopy during unstable conditions: identification of episodes using wavelet analysis. J Geophys Res D 106:7251–7262. https://doi.org/10.1029/2000JD900662CrossRef

Schatzmann M, König G, Lohmeyer A (1986) Physikalische Modellierung mikrometeorologischer Vorgänge im Windkanal. Meteorol Rundschau 39:44–59

Schlegel F, Stiller J, Bienert A, Maas H-G, Queck R, Bernhofer C (2012) Large-Eddy simulation of inhomogeneous canopy flows using high resolution terrestrial laser scanning data. Boundary-Layer Meteorol 142:223–243. https://doi.org/10.1007/s10546-011-9678-1CrossRef

Schlegel F, Stiller J, Bienert A, Maas H-G, Queck R, Bernhofer C (2015) Large-Eddy Simulation study of the effects on flow of a heterogeneous forest at sub-tree resolution. Boundary-Layer Meteorol 154:27–56. https://doi.org/10.1007/s10546-014-9962-yCrossRef

Schmid HP (1994) Source areas for scalars and scalar fluxes. Boundary-Layer Meteorol 67:293–318. https://doi.org/10.1007/BF00713146CrossRef

Schmid HP (1997) Experimental design for flux measurements: matching scales of observations and fluxes. Agric For Meteorol 87:179–200. https://doi.org/10.1016/S0168-1923(97)00011-7CrossRef

Schmid HP (2002) Footprint modeling for vegetation atmosphere exchange studies: a review and perspective. Agric For Meteorol 113:159–184. https://doi.org/10.1016/S0168-1923(02)00107-7CrossRef

Schmid HP, Bünzli D (1995) The influence of the surface texture on the effective roughness length. Quart J R Meteorol Soc 121:1–21. https://doi.org/10.1002/qj.49712152102CrossRef

Schmid HP, Oke TR (1988) Estimating the source area of a turbulent flux measurement over a patchy surface. In: 8^th Symposium on Turbulence and Diffusion, San Diego, CA., April 26–29, 1988. Am Meteorol Soc, S 123–126

Schmid HP, Oke TR (1990) A model to estimate the source area contributing to turbulent exchange in the surface layer over patchy terrain. Quart J R Meteorol Soc 116:965–988. https://doi.org/10.1002/qj.49711649409CrossRef

Schuepp PH, Leclerc MY, MacPherson JI, Desjardins RL (1990) Footprint prediction of scalar fluxes from analytical solutions of the diffusion equation. Boundary-Layer Meteorol 50:355–373. https://doi.org/10.1007/BF00120530CrossRef

Serafimovich A, Thomas C, Foken T (2011) Vertical and horizontal transport of energy and matter by coherent motions in a tall spruce canopy. Boundary-Layer Meteorol 140:429–451. https://doi.org/10.1007/s10546-011-9619-zCrossRef

Serafimovich A, Hübner J, Leclerc MJ, Duarte HF, Foken T (2017) Influence of low-level jets and gravity waves on turbulent fluxes. In: Foken T (ed) Energy and matter fluxes of a spruce forest ecosystem, Ecological studies, vol 229. Springer, Cham, pp 247–276. https://doi.org/10.1007/978-3-319-49389-3_11CrossRef

Serafimovich A, Metzger S, Hartmann J, Kohnert K, Zona D, Sachs T (2018) Upscaling surface energy fluxes over the North Slope of Alaska using airborne eddy-covariance measurements and environmental response functions. Atmos Chem Phys 18:10007–10023. https://doi.org/10.5194/acp-18-10007-2018CrossRef

Shapkalijevski MM, Ouwersloot HG, Moene AF, de Arrellano JVG (2017) Integrating canopy and large-scale effects in the convective boundary-layer dynamics during the CHATS experiment. Atmos Chem Phys 17(3):1623–1640. https://doi.org/10.5194/acp-17-1623-2017CrossRef

Shaw RH (1977) Secondary wind speed maxima inside plant canopies. J Appl Meteorol 16:514–521. https://doi.org/10.1175/1520-0450(1977)016<0514:SWSMIP>2.0.CO;2CrossRef

Shaw RH, Silversides RH, Thurtell GW (1974) Some observations of turbulence and turbulent transport within and above plant canopies. Boundary-Layer Meteorol 5:429–449. https://doi.org/10.1007/BF00123490CrossRef

Shaw RH, Tavangar J, Ward DP (1983) Structure of the Reynolds stress in a canopy layer. J Clim Appl Meteorol 22:1922–1931. https://doi.org/10.1175/1520-0450(1983)022<1922:SOTRSI>2.0.CO;2CrossRef

Shen S, Leclerc MY (1994) Large-eddy simulation of small scale surface effects on the convective boundary layer structure. Atmosphere-Ocean 32:717–731. https://doi.org/10.1002/qj.49712152603CrossRef

Shir CC (1972) A numerical computation of the air flow over a sudden change of surface roughness. J Atmos Sci 29:304–310. https://doi.org/10.1175/1520-0469(1972)029<0304:ANCOAF>2.0.CO;2CrossRef

Shuttleworth WJ (1989) Micrometeorology of temperate and tropical forest. Phil Trans R Soc Lond B 324:299–334. https://doi.org/10.1098/rstb.1989.0050CrossRef

Simpson IJ, Thurtell GW, Neumann HH, Hartog GD, Edwards GC (1998) The validity of similarity theory in the roughness sublayer above forests. Boundary-Layer Meteorol 87:69–99. https://doi.org/10.1023/A:1000809902980CrossRef

Sodemann H, Foken T (2005) Special characteristics of the temperature structure near the surface. Theor Appl Climat 80:81–89. https://doi.org/10.1007/s00704-004-0092-1CrossRef

Sogachev A, Lloyd J (2004) Using a one-and-a-half order closure model of atmospheric boundary layer for surface flux footprint estimation. Boundary-Layer Meteorol 112:467–502. https://doi.org/10.1023/B:BOUN.0000030664.52282.eeCrossRef

Spirig C, Ammann C, Neftel A (2017) ART Footprint Tool. Zenodo 816236. https://doi.org/10.5281/zenodo.816236

Staudt K, Serafimovich A, Siebicke L, Pyles RD, Falge E (2011) Vertical structure of evapotranspiration at a forest site (a case study). Agric For Meteorol 151:709–729. https://doi.org/10.1016/j.agrformet.2010.10.009CrossRef

Steinfeld G, Raasch S, Markkanen T (2008) Footprints in homogeneously and heterogeneously driven boundary layers derived from a Lagrangian stochastic particle model embedded into large-eddy simulation. Boundary-Layer Meteorol 129:225–248. https://doi.org/10.1007/s10546-008-9317-7CrossRef

Stull RB (1988) An introduction to Boundary Layer meteorology. Kluwer, Dordrecht. https://doi.org/10.1007/978-94-009-3027-8CrossRef

Sühring M, Raasch S (2013) Heterogeneity-induced heat-flux patterns in the convective boundary layer: can they be detected from observations and is there a blending height?—A Large-Eddy simulation study for the LITFASS-2003 experiment. Boundary-Layer Meteorol 148:309–331. https://doi.org/10.1007/s10546-013-9822-1CrossRef

Taylor PA (1969) On wind and shear stress profiles above a change in surface roughness. Quart J R Meteorol Soc 95:77–91. https://doi.org/10.1002/qj.49709540306CrossRef

Taylor PA (1987) Comments and further analysis on the effective roughness length for use in numerical three-dimensional models: a research note. Boundary-Layer Meteorol 39:403–418. https://doi.org/10.1007/BF00125144CrossRef

Thom AS, Stewart JB, Oliver HR, Gash JHC (1975) Comparison of aerodynamic and energy budget estimates of fluxes over a pine forest. Quart J R Meteorol Soc 101:93–105. https://doi.org/10.1002/qj.49710142708CrossRef

Thomas CK (2011) Variability of sub-canopy flow, temperature, and horizontal advection in moderately complex terrain. Boundary-Layer Meteorol 139:61–81. https://doi.org/10.1007/s10546-010-9578-9CrossRef

Thomas C, Foken T (2005) Detection of long-term coherent exchange over spruce forest. Theor Appl Climat 80:91–104. https://doi.org/10.1007/s00704-004-0093-0CrossRef

Thomas C, Foken T (2007a) Organised motion in a tall spruce canopy: temporal scales, structure spacing and terrain effects. Boundary-Layer Meteorol 122:123–147. https://doi.org/10.1007/s10546-006-9087-zCrossRef

Thomas C, Foken T (2007b) Flux contribution of coherent structures and its implications for the exchange of energy and matter in a tall spruce canopy. Boundary-Layer Meteorol 123:317–337. https://doi.org/10.1007/s10546-006-9144-7CrossRef

Thomas CK, Selker J (2021) Optical-fiber-based distributed sensing methods. In: Foken T (ed) Springer handbook of atmospheric measurements. Springer Nature, Bern, pp 609–631. https://doi.org/10.1007/978-3-030-52171-4_20CrossRef

Thomas C, Martin JG, Göckede M, Siqueira MB, Foken T, Law BE, Loescher HW, Katul G (2008) Estimating daytime subcanopy respiration from conditional sampling methods applied to multi-scalar high frequency turbulence time series. Agric For Meteorol 148:1210–1229. https://doi.org/10.1016/j.agrformet.2008.03.002CrossRef

Thomas CK, Kennedy AM, Selker JS, Moretti A, Schroth MH, Smoot AR, Tufillaro NB, Zeeman MJ (2012) High-resolution fibre-optic temperature sensing: a new tool to study the two-dimensional structure of atmospheric surface-layer flow. Boundary-Layer Meteorol 142:177–192. https://doi.org/10.1007/s10546-011-9672-7CrossRef

Thomas CK, Martin JG, Law BE, Davis K (2013) Toward biologically meaningful net carbon exchange estimates for tall, dense canopies: multi-level eddy covariance observations and canopy coupling regimes in a mature Douglas-fir forest in Oregon. Agric For Meteorol 173:14–27. https://doi.org/10.1016/j.agrformet.2013.01.001CrossRef

Thomas CK, Serafimovich A, Siebicke L, Gerken T, Foken T (2017) Coherent structures and flux coupling. In: Foken T (ed) Energy and matter fluxes of a spruce forest ecosystem, Ecological studies, vol 229. Springer, Cham, pp 113–135. https://doi.org/10.1007/978-3-319-49389-3_6CrossRef

Torrence C, Compo GP (1998) A practical guide to wavelet analysis. Bull Am Meteorol Soc 79:61–78. https://doi.org/10.1175/1520-0477(1998)079<0061:APGTWA>2.0.CO;2CrossRef

Troen I, Lundtang Petersen E (1989) European Wind Atlas. Risø National Laboratory, Roskilde

Twine TE, Kustas WP, Norman JM, Cook DR, Houser PR, Meyers TP, Prueger JH, Starks PJ, Wesely ML (2000) Correcting eddy-covariance flux underestimates over a grassland. Agric For Meteorol 103:279–300. https://doi.org/10.1016/S0168-1923(00)00123-4CrossRef

VDI (2018) Umweltmeteorologie, meteorologische messungen, wind (Environmental meteorology, meteorological measurements, wind), VDI 3786, Blatt (Part) 2. Beuth Verlag, Berlin

Venditti JG, Best JL, Church M, Hardy RJ (2013) Coherent flow structures at earth’s surface. Wiley, ChichesterCrossRef

Verhoef A, McNaughton KG, Jacobs AFG (1997) A parameterization of momentum roughness length and displacement height for a wide range of canopy densities. Hydrol Earth Syst Sci 1:81–91. https://doi.org/10.5194/hess-1-81-1997CrossRef

Vesala T, Kljun N, Rannik U, Rinne J, Sogachev A, Markkanen T, Sabelfeld K, Foken T, Leclerc MY (2008) Flux and concentration footprint modelling: state of the art. Environ Pollut 152:653–666. https://doi.org/10.1016/j.envpol.2007.06.070CrossRef

Wanner L, Calaf M, Mauder M (2022) Incorporating the effect of heterogeneous surface heating into a semi-empirical model of the surface energy balance closure PLOS ONE 17: e0268097. https://doi.org/10.1371/journal.pone.0268097

Waterhouse FL (1955) Micrometeorological profiles in grass cover in relation to biological problems. Quart J R Meteorol Soc 81:63–71. https://doi.org/10.1002/qj.49708134707CrossRef

Webb EK, Pearman GI, Leuning R (1980) Correction of the flux measurements for density effects due to heat and water vapour transfer. Quart J R Meteorol Soc 106:85–100. https://doi.org/10.1002/qj.49710644707CrossRef

Wichura B, Buchmann N, Foken T, Mangold A, Heinz G, Rebmann C (2001) Pools und Flüsse des stabilen Kohlenstoffisotops ¹³C zwischen Boden, Vegetation und Atmosphäre in verschiedenen Pflanzengemeinschaften des Fichtelgebirges. Bayreuther Forum Ökologie 84:123–153

Wilson JD, Ward DP, Thurtell GW, Kidd GE (1982) Statistics of atmospheric turbulence within and above a corn canopy. Boundary-Layer Meteorol 24:495–519. https://doi.org/10.1007/BF00120736CrossRef

Wilson KB, Goldstein AH, Falge E, Aubinet M, Baldocchi D, Berbigier P, Bernhofer C, Ceulemans R, Dolman H, Field C, Grelle A, Law B, Meyers T, Moncrieff J, Monson R, Oechel W, Tenhunen J, Valentini R, Verma S (2002) Energy balance closure at FLUXNET sites. Agric For Meteorol 113:223–234. https://doi.org/10.1016/S0168-1923(02)00109-0CrossRef

WMO (1981) Meteorological aspects of the utilization of wind as an energy source, Bd 175. WMO, Technical Note

Xu K, Metzger S, Desai AR (2017) Upscaling tower-observed turbulent exchange at fine spatio-temporal resolution using environmental response functions. Agric For Meteorol 232:10–22. https://doi.org/10.1016/j.agrformet.2016.07.019CrossRef

Xu K, Sühring M, Metzger S, Durden D, Desai A (2020) Can data mining help Eddy covariance see the landscape? A Large-Eddy simulation study. Boundary-Layer Meteorol 176:85–103. https://doi.org/10.1007/s10546-020-00513-0CrossRef

Yi C (2008) Momentum transfer within canopies. J Appl Meteorol Climatol 47:262–275. https://doi.org/10.1175/2007JAMC1667.1CrossRef

Zelený J, Foken T (1991) Ausgewählte Ergebnisse des Grenzschichtexperimentes in Bohunice 1989. Z Meteorol 41:439–445

Zelený J, Pretel J (1986) Zur Problematik der Bestimmung der aerodynamischen Rauhigkeit der Erdoberfläche. Z Meteorol 36:325

Zhang G, Thomas C, Leclerc MY, Karipot A, Gholz HL, Foken T (2007) On the effect of clearcuts on turbulence structure above a forest canopy. Theor Appl Climat 88:133–137. https://doi.org/10.1007/s00704-006-0250-8CrossRef

Zilitinkevich SS, Calanca P (2000) An extended similarity theory for the stably stratified atmospheric surface layer. Quart J R Meteorol Soc 126:1913–1923. https://doi.org/10.1002/qj.49712656617CrossRef

Zilitinkevich SS, Perov VL, King JC (2002) Near-surface turbulent fluxes in stable stratification: Calculation techniques for use in general circulation models. Quart J R Meteorol Soc 128:1571–1587. https://doi.org/10.1002/qj.200212858309CrossRef

Zilitinkevich SS, Elperin T, Kleeorin N, Rogachevskii I, Esau I (2013) A Hierarchy of Energy- and Flux-Budget (EFB) turbulence closure models for stably-stratified geophysical flows. Boundary-Layer Meteorol 146:341–373. https://doi.org/10.1007/s10546-012-9768-8CrossRef

Zubkovskij SL, Sushko AA (1987) Eksperimentalnoe issledovanie prostranstvennoj struktury temperaturnogo polja v prizemnom sloe atmosfery (Experimental investigations spatial structure of the temperature field in the near surface layer of the atmosphere). Meteorol Issledovanija 28:36–41

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