The role of land–atmosphere coupling in subseasonal surface air temperature prediction across the contiguous United States

<p>Land–atmosphere (L–A) coupling can play a crucial role for subseasonal-to-seasonal (S2S) predictability and prediction. When coupling is strong, L–A processes and feedback are expected to enhance the system's memory, thereby increasing the predictability and prediction skill. This stud...

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Main Authors: Y. Lim, A. M. Molod, R. D. Koster, J. A. Santanello
Format: Article
Language:English
Published: Copernicus Publications 2025-08-01
Series:Hydrology and Earth System Sciences
Online Access:https://hess.copernicus.org/articles/29/3435/2025/hess-29-3435-2025.pdf
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author Y. Lim
Y. Lim
A. M. Molod
R. D. Koster
J. A. Santanello
author_facet Y. Lim
Y. Lim
A. M. Molod
R. D. Koster
J. A. Santanello
author_sort Y. Lim
collection DOAJ
description <p>Land–atmosphere (L–A) coupling can play a crucial role for subseasonal-to-seasonal (S2S) predictability and prediction. When coupling is strong, L–A processes and feedback are expected to enhance the system's memory, thereby increasing the predictability and prediction skill. This study evaluates the subseasonal prediction of ambient surface air temperature under conditions of strong versus weak L–A coupling in forecasts produced with NASA's state-of-the-art Goddard Earth Observing System (GEOS) S2S forecast system. By applying three L–A coupling metrics that collectively capture the connection between the soil and the free troposphere, we observe improved prediction skill for surface air temperature during weeks 3–4 of boreal summer forecasts across the Midwest and northern Great Plains, particularly when all three indices indicate strong L–A coupling at this lead time. The prediction skill indeed increases as more indices show strong coupling. The forecasts with strong L–A coupling in these regions tend to exhibit sustained warm and dry anomalies, signals that are well simulated in the model. Overall, this study highlights how better identifying and capturing relevant L–A coupling processes can potentially enhance prediction on S2S timescales.</p>
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publishDate 2025-08-01
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spelling doaj-art-668c00513f814b28a6ecf9582f7cd6822025-08-20T03:15:55ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382025-08-01293435344510.5194/hess-29-3435-2025The role of land–atmosphere coupling in subseasonal surface air temperature prediction across the contiguous United StatesY. Lim0Y. Lim1A. M. Molod2R. D. Koster3J. A. Santanello4Earth System Science Interdisciplinary Center, University of Maryland College Park, College Park, Maryland 20740, USAGlobal Modeling and Assimilation Office, NASA Goddard Space Flight Center, Greenbelt, Maryland 20771, USAGlobal Modeling and Assimilation Office, NASA Goddard Space Flight Center, Greenbelt, Maryland 20771, USAGlobal Modeling and Assimilation Office, NASA Goddard Space Flight Center, Greenbelt, Maryland 20771, USAHydrological Sciences Laboratory, NASA Goddard Space Flight Center, Greenbelt, Maryland 20771, USA<p>Land–atmosphere (L–A) coupling can play a crucial role for subseasonal-to-seasonal (S2S) predictability and prediction. When coupling is strong, L–A processes and feedback are expected to enhance the system's memory, thereby increasing the predictability and prediction skill. This study evaluates the subseasonal prediction of ambient surface air temperature under conditions of strong versus weak L–A coupling in forecasts produced with NASA's state-of-the-art Goddard Earth Observing System (GEOS) S2S forecast system. By applying three L–A coupling metrics that collectively capture the connection between the soil and the free troposphere, we observe improved prediction skill for surface air temperature during weeks 3–4 of boreal summer forecasts across the Midwest and northern Great Plains, particularly when all three indices indicate strong L–A coupling at this lead time. The prediction skill indeed increases as more indices show strong coupling. The forecasts with strong L–A coupling in these regions tend to exhibit sustained warm and dry anomalies, signals that are well simulated in the model. Overall, this study highlights how better identifying and capturing relevant L–A coupling processes can potentially enhance prediction on S2S timescales.</p>https://hess.copernicus.org/articles/29/3435/2025/hess-29-3435-2025.pdf
spellingShingle Y. Lim
Y. Lim
A. M. Molod
R. D. Koster
J. A. Santanello
The role of land–atmosphere coupling in subseasonal surface air temperature prediction across the contiguous United States
Hydrology and Earth System Sciences
title The role of land–atmosphere coupling in subseasonal surface air temperature prediction across the contiguous United States
title_full The role of land–atmosphere coupling in subseasonal surface air temperature prediction across the contiguous United States
title_fullStr The role of land–atmosphere coupling in subseasonal surface air temperature prediction across the contiguous United States
title_full_unstemmed The role of land–atmosphere coupling in subseasonal surface air temperature prediction across the contiguous United States
title_short The role of land–atmosphere coupling in subseasonal surface air temperature prediction across the contiguous United States
title_sort role of land atmosphere coupling in subseasonal surface air temperature prediction across the contiguous united states
url https://hess.copernicus.org/articles/29/3435/2025/hess-29-3435-2025.pdf
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