Deducing land-atmosphere coupling regimes from SMAP soil moisture

• Published in: Hydrology and earth system sciences 2024-11, Vol.28 (22), p.5087-5106
• Main Authors: Makhasana, Payal R, Santanello, Joseph A, Lawston-Parker, Patricia M, Roundy, Joshua K
• Format: Article
• Language: English
• Subjects: Atmosphere; Classification; Coupling; Datasets; Dew; Drought; Drought monitoring; Environmental monitoring; Estimates; Humidity; Humidity indexes; Integrated approach; Land surface models; Moisture content; Noise prediction; Precipitation; Radiosondes; Random noise; Remote sensing; Satellite observation; Soil; Soil moisture; Soil moisture variations; Soil strength; Soil water; Strength; Variables
• ISSN: 1027-5606; 1607-7938
• DOI: 10.5194/hess-28-5087-2024

In recent years, there has been a growing recognition of the significance of land-atmosphere (L-A) interactions and feedback mechanisms in understanding and predicting Earth's water and energy cycles. Soil moisture plays a critical role in mediating the strength of L-A interactions and is important for understanding the complex and governing processes across this interface. This study aims to identify the significance of soil moisture in identifying L-A coupling strength within the convective triggering potential (CTP) and humidity index (HI) framework. To address this, a consistent and reliable dataset of atmospheric profiles is created by merging CTP and HI using triple collocation (TC) with three reanalysis datasets. The merged CTP and HI product demonstrates enhanced performance globally compared to the individual datasets when validated with radiosonde and satellite observations. This merged product of CTP and HI is then used to compare the L-A coupling strength based on Soil Moisture Active Passive Level 3 (SMAPL3) and SMAP Level 4 (SMAPL4) over 2 decades (2003-2022) where L-A coupling strength is defined as the persistence probability within the dry and wet coupling regimes. Results indicate that the persistency-based coupling strength is related to the ability of soil moisture to predict future atmospheric humidity and dry vs. wet coupling state. The coupling strength in SMAPL4 is consistently stronger than in SMAPL3 and is likely due to its reliance on a land surface model and reduced susceptibility to random noise. The difference in coupling strength based on the same CTP-HI underscores the importance of soil moisture data in estimating coupling strength within the CTP-HI framework. These findings lay the groundwork for understanding the role of L-A interactions and drought evolution due to soil moisture variations by providing insight into the quantification of coupling strength and its role in drought monitoring and forecast efforts.