GSTDTAP  > 地球科学
DOI10.5194/acp-18-10007-2018
Upscaling surface energy fluxes over the North Slope of Alaska using airborne eddy-covariance measurements and environmental response functions
Serafimovich, Andrei1; Metzger, Stefan2,3; Hartmann, Joerg4; Kohnert, Katrin1; Zona, Donatella5,6; Sachs, Torsten1,7
2018-07-13
发表期刊ATMOSPHERIC CHEMISTRY AND PHYSICS
ISSN1680-7316
EISSN1680-7324
出版年2018
卷号18期号:13页码:10007-10023
文章类型Article
语种英语
国家Germany; USA; England
英文摘要

The objective of this study was to upscale airborne flux measurements of sensible heat and latent heat and to develop high-resolution flux maps. In order to support the evaluation of coupled atmospheric-land-surface models we investigated spatial patterns of energy fluxes in relation to land-surface properties.


We used airborne eddy-covariance measurements acquired by the Polar 5 research aircraft in June-July 2012 to analyze surface fluxes. Footprint-weighted surface properties were then related to 21 529 sensible heat flux observations and 25 608 latent heat flux observations using both remote sensing and modeled data. A boosted regression tree technique was used to estimate environmental response functions between spatially and temporally resolved flux observations and corresponding biophysical and meteorological drivers. In order to improve the spatial coverage and spatial representativeness of energy fluxes we used relationships extracted across heterogeneous Arctic landscapes to infer high-resolution surface energy flux maps, thus directly upscaling the observational data. These maps of projected sensible heat and latent heat fluxes were used to assess energy partitioning in northern ecosystems and to determine the dominant energy exchange processes in permafrost areas. This allowed us to estimate energy fluxes for specific types of land cover, taking into account meteorological conditions. Airborne and modeled fluxes were then compared with measurements from an eddy-covariance tower near Atqasuk.


Our results are an important contribution for the advanced, scale-dependent quantification of surface energy fluxes and they provide new insights into the processes affecting these fluxes for the main vegetation types in high-latitude permafrost areas.


领域地球科学
收录类别SCI-E
WOS记录号WOS:000438536200007
WOS关键词POLYGONAL TUNDRA SITE ; BOREAL FOREST ; CARBON-DIOXIDE ; ARCTIC TUNDRA ; AIRCRAFT ; CLIMATE ; TOWER ; BALANCE ; FEEDBACKS ; VEGETATION
WOS类目Environmental Sciences ; Meteorology & Atmospheric Sciences
WOS研究方向Environmental Sciences & Ecology ; Meteorology & Atmospheric Sciences
引用统计
文献类型期刊论文
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/30760
专题地球科学
作者单位1.Helmholtz Ctr Potsdam, GFZ German Res Ctr Geosci, D-14473 Potsdam, Germany;
2.Natl Ecol Observ Network, Fundamental Instrument Unit, 1685 38th St, Boulder, CO 80301 USA;
3.Univ Wisconsin, Dept Atmospher & Ocean Sci, 1225 West Dayton St, Madison, WI 53706 USA;
4.Helmholtz Ctr Polar & Marine Res AWI, Alfred Wegener Inst, Handelshafen 12, D-27570 Bremerhaven, Germany;
5.Univ Sheffield, Dept Anim & Plant Sci, Western Bank, Sheffield S10 2TN, S Yorkshire, England;
6.San Diego State Univ, Dept Biol, 5500 Campanile Dr, San Diego, CA 92182 USA;
7.TU Braunschweig, Inst Flight Guidance, Hermann Blenk Str 27, D-38108 Braunschweig, Germany
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Serafimovich, Andrei,Metzger, Stefan,Hartmann, Joerg,et al. Upscaling surface energy fluxes over the North Slope of Alaska using airborne eddy-covariance measurements and environmental response functions[J]. ATMOSPHERIC CHEMISTRY AND PHYSICS,2018,18(13):10007-10023.
APA Serafimovich, Andrei,Metzger, Stefan,Hartmann, Joerg,Kohnert, Katrin,Zona, Donatella,&Sachs, Torsten.(2018).Upscaling surface energy fluxes over the North Slope of Alaska using airborne eddy-covariance measurements and environmental response functions.ATMOSPHERIC CHEMISTRY AND PHYSICS,18(13),10007-10023.
MLA Serafimovich, Andrei,et al."Upscaling surface energy fluxes over the North Slope of Alaska using airborne eddy-covariance measurements and environmental response functions".ATMOSPHERIC CHEMISTRY AND PHYSICS 18.13(2018):10007-10023.
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