Regional Moisture Budget and Land‐Atmosphere Coupling Over the U.S. Southern Great Plains Inferred From the ARM Long‐Term Observations. Issue 17 (4th September 2019)

• Record Type: Journal Article
• Authors: Tao, Cheng; Zhang, Yunyan; Tang, Shuaiqi; Tang, Qi; Ma, Hsi‐Yen; Xie, Shaocheng; Zhang, Minghua
• Is Part Of: Journal of geophysical research. Volume 124:Issue 17/18(2019)
• Page Start: 10091
• Page End: 10108
• Publication Date: 2019-09-04
• Subjects: Atmospheric physics -- Periodicals; Geophysics -- Periodicals; 551.5
• DOI: 10.1029/2019JD030585
• Languages: English
• ISSNs: 2169-897X

Abstract

Abstract: Ten‐year warm‐season (May–August) observations at the Atmospheric Radiation Measurement (ARM) Southern Great Plains (SGP) site are used to examine the large‐scale atmospheric moisture budget and the strength of land‐atmosphere coupling. Atmospheric moisture budget components, computed from the ARM variational analysis data, are compared between different wet/dry scenarios and convection regimes. Consistent with previous studies, large‐scale moisture flux convergence dominates the SGP regional moisture budget on the daily time scale, but surface evaporation does play a more prominent role on late‐afternoon deep convection days. Moreover, the relationship between moisture flux convergence and precipitation increases significantly from dry year to wet years. The land‐atmosphere coupling strength is quantified for local convective events within the "Local L‐A Coupling Process Chain" (Santanello et al., 2018, https://doi.org/10.1175/BAMS‐D‐17‐0001.1 ). The impact of land surface on the evolution of planetary boundary layer is highly dependent on the vegetation leaf area index. A significantly larger surface sensible heat flux is found over the SGP forest region in midsummer, which is accompanied by a much higher planetary boundary layer development and a large increase in shallow cumulus cloud fraction. The significant relationship between afternoon precipitation and surface turbulent flux only exists in the northeast part of the ARM SGP site, which is mainly covered by grassland/pasture. Key Points: Surface evaporation (moisture flux convergence) is the dominant moisture source for late‐afternoon (nighttime) deep convection The land surface control on the evolution of atmospheric boundary layer is dependent on vegetation leaf area index A much higher cloud fraction is found over forest than over grassland on fair‐weather shallow cumulus days