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Partitioning of Sensible and Latent Heat Fluxes in Different Vegetation Types and Their Spatiotemporal Variations Based on 203 FLUXNET Sites.

Authors :
Lin, Huiqing
Li, Yan
Zhao, Lei
Source :
Journal of Geophysical Research. Atmospheres; 11/16/2022, Vol. 127 Issue 21, p1-13, 13p
Publication Year :
2022

Abstract

Bowen ratio reflects the partitioning between sensible and latent heat fluxes and plays a crucial role in land–atmosphere interaction. In this study, the spatiotemporal variations of Bowen ratio among 12 vegetation types were analyzed using observations from 203 FLUXNET sites and compared against Community Land Model (CLM) simulations. Results showed that the annual mean Bowen ratio across all sites was 1.48 ± 1.20 (mean ± SD). Sites with Bowen ratios less than 1 were found across all continents, and the ones with a higher Bowen ratio appeared in dry and warm areas. Open shrublands showed the highest Bowen ratio (3.04 ± 0.58), whereas wetlands showed the lowest (0.74 ± 0.09). In terms of seasonality, Bowen ratio generally showed lower values in local summer and higher in spring and autumn in the northern hemisphere; the opposite occurred in the southern hemisphere. The spatiotemporal variations in Bowen ratio can be explained by climatic, geographical, and biological factors, with climate factors having the greatest impact. The spatial correlation analyses suggested Bowen ratio increased under higher VPD (R = 0.45, p < 0.001) and hotter (R = 0.14, p < 0.05) conditions and decreased with higher precipitation (R = −0.34, p < 0.001), albedo (R = −0.16, p > 0.05), and leaf area index (R = −0.25, p < 0.001). Compared to FLUXNET observations, CLM well reproduced the global annual mean Bowen ratio (1.48 for CLM vs. 1.56 for FLUXNET) but showed larger differences for certain vegetation types. Our results could enhance our understanding of biotic and environmental controls on land surface energy fluxes and help improve the land surface and climate models. Key Points: Open shrublands showed the highest Bowen ratio, followed by savannas, grasslands, forests, and croplands, and the lowest in wetlandsThe spatiotemporal variations in Bowen ratio can be explained by climatic, geographical, and biological factors, especially climate factorsCommunity Land Model well captured the global annual mean Bowen ratio but showed large differences for certain vegetation types [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
2169897X
Volume :
127
Issue :
21
Database :
Complementary Index
Journal :
Journal of Geophysical Research. Atmospheres
Publication Type :
Academic Journal
Accession number :
160149138
Full Text :
https://doi.org/10.1029/2022JD037142