Rain‐Induced Stratification of the Equatorial Indian Ocean and Its Potential Feedback to the Atmosphere
Author:
Affiliation:
1. Department of Atmospheric Science Colorado State University Fort Collins CO USA
2. Department of Meteorology University of Reading Reading UK
3. NOAA Physical Sciences Lab Boulder CO USA
4. Pacific Northwest National Laboratory Richland WA USA
Funder
National Science Foundation
H2020 European Research Council
Publisher
American Geophysical Union (AGU)
Subject
Earth and Planetary Sciences (miscellaneous),Space and Planetary Science,Geochemistry and Petrology,Geophysics,Oceanography
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021JC018025
Reference60 articles.
1. Observations of rain-induced near-surface salinity anomalies
2. On the Relationship between SST Gradients, Boundary Layer Winds, and Convergence over the Tropical Oceans
3. A Simple Model of Climatological Rainfall and Vertical Motion Patterns over the Tropical Oceans
4. An Analysis of Tropical Ocean Diurnal Warm Layers
5. Role of Diurnal Warm Layers in the Diurnal Cycle of Convection over the Tropical Indian Ocean during MISMO
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