气候变化领域集成服务门户(CCPortal): Cold Pool Responses to Changes in Soil Moisture

CCPortal

DOI	10.1029/2019MS001922
	Cold Pool Responses to Changes in Soil Moisture
	Drager A.J.; Grant L.D.; van den Heever S.C.
发表日期	2020
ISSN	19422466
卷号	12 期号:8
英文摘要	This study examines the role of soil moisture in modulating convective cold pool properties in an idealized modeling framework that uses a cloud-resolving model coupled to an interactive land surface model. Five high-resolution simulations of tropical continental convection are conducted in which the initial soil moisture is varied. The hundreds of cold pools forming within each simulation are identified and composited across space and time using an objective cold pool identification algorithm. Several important findings emerge from this analysis. Lower soil moisture results in greater daytime heating of the surface, which produces a deeper, drier subcloud layer. As a result, latent cooling through the evaporation of precipitation is enhanced, and cold pools are stronger and deeper. Increased propagation speed, combined with wider rain shafts, results in wider cold pools. Finally, the rings of enhanced water vapor that surround each cold pool when soil is wet disappear when the soil moisture is reduced, due to the suppression of surface latent heat fluxes. Instead, short-lived “puddles” of enhanced water vapor permeate the cold pools. The results are nonlinear in that the properties of the cold pools in the two driest-soil simulations depart substantially from the cold pool properties in the three simulations initialized with wetter soil. The dividing line between the resulting wet-soil and dry-soil regimes is the permanent wilting point. Below the permanent wilting point, transpiration is subdued due to a sharp increase in water stress. These results emphasize the role of land surface-boundary layer-cloud interactions in modulating cold pool properties. © 2020. The Authors.
英文关键词	cold pools; convection; density currents; soil moisture
语种	英语
scopus关键词	Boundary layer flow; Boundary layers; Soil moisture; Surface measurement; Water vapor; Cloud resolving model; High resolution simulations; Identification algorithms; Initial soil moisture; Land surface boundary layers; Land surface modeling; Permanent wilting points; Surface latent heat fluxes; Lakes; atmospheric convection; cold pool; evaporation; evapotranspiration; land surface; soil moisture
来源期刊	Journal of Advances in Modeling Earth Systems
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/156660
作者单位	Department of Atmospheric Science, Colorado State University, Fort Collins, CO, United States
推荐引用方式 GB/T 7714	Drager A.J.,Grant L.D.,van den Heever S.C.. Cold Pool Responses to Changes in Soil Moisture[J],2020,12(8).
APA	Drager A.J.,Grant L.D.,&van den Heever S.C..(2020).Cold Pool Responses to Changes in Soil Moisture.Journal of Advances in Modeling Earth Systems,12(8).
MLA	Drager A.J.,et al."Cold Pool Responses to Changes in Soil Moisture".Journal of Advances in Modeling Earth Systems 12.8(2020).