Effects of Lake Baikal on Summertime Precipitation Climatology Over the Lake Surface

Author:

Lee Hyunho1ORCID,Ganbat Gantuya2ORCID,Jin Han‐Gyul3ORCID,Seo Jaemyeong Mango4ORCID,Moon Sungju5ORCID,Bok Hyejeong6,Baik Jong‐Jin3ORCID

Affiliation:

1. Department of Atmospheric Science Kongju National University Gongju South Korea

2. Faculty of Raw Materials and Environmental Engineering German‐Mongolian Institute for Resources and Technology Ulaanbaatar Mongolia

3. School of Earth and Environmental Sciences Seoul National University Seoul South Korea

4. Max‐Planck Institute for Meteorology Hamburg Germany

5. Department of Data, Media, and Design Nevada State College Henderson NV USA

6. Numerical Modeling Center Korea Meteorological Administration Daejeon South Korea

Abstract

AbstractThis study investigates the impacts of Lake Baikal, the largest by volume and the deepest freshwater lake in the world, on its nearby precipitation climate. Satellite observations and a reanalysis data set reveal that summertime precipitation amount is smaller over Lake Baikal than around it. A 15‐year regional climate simulation at a cloud‐resolving scale supports the smaller precipitation, and another simulation in which the lake is replaced by forest shows that the lake reduces summertime precipitation over it by 15%. The lake decreases daytime near‐surface air temperature, resulting in more convectively stable atmosphere over the lake. Latent heat flux is reduced along with the weakened convection, and the lower‐level moisture convergence and upper‐level moisture divergence over the lake are weakened.

Funder

National Research Foundation of Korea

Kongju National University

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

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