4.7 Article

Interannual Variation of the Spring and Summer Precipitation over the Three River Source Region in China and the Associated Regimes

Journal

JOURNAL OF CLIMATE
Volume 31, Issue 18, Pages 7441-7457

Publisher

AMER METEOROLOGICAL SOC
DOI: 10.1175/JCLI-D-17-0680.1

Keywords

Atmospheric circulation; Dynamics; ENSO; Hydrologic cycle; Teleconnections; Interannual variability

Funding

  1. National Key Research and Development Plan [2016YFA0600703]
  2. Natural Science Foundation of Jiangsu Province of China [SBK2018040337]
  3. Jiangsu Innovation and Entrepreneurship Team
  4. Priority Academic Program Development of Jiangsu Higher Education Institutions (PAPD)
  5. CAS-PKU Partnership Program

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This study analyzes the interannual and interdecadal variability of spring and summer precipitation over the Three River Source (TRS) region in China using four datasets. A general consistency is revealed among the four datasets with regard to the interannual and interdecadal variability of TRS precipitation during 1979-2015, demonstrating a confidence of the four datasets in representing the precipitation variability over the TRS region. The TRS spring and summer precipitation shows distinct interannual and interdecadal variability, with an overall increasing trend in the spring precipitation and an interdecadal oscillation in the summer precipitation. The regimes associated with the interannual variability of TRS spring and summer precipitation are further investigated. The interannual variability of TRS spring precipitation is essentially modulated by an anomalous easterly water vapor transport (WVT) branch associated with the leading mode of Eurasian spring circulation. El Nino-Southern Oscillation (ENSO) may affect the interannual variability of TRS spring precipitation by causing southerly WVT anomalies toward the TRS region. The interannual variability of TRS summer precipitation is essentially modulated by an anomalous southwesterly WVT branch over the TRS region, which is mainly associated with a Eurasian wave train connected with the summer North Atlantic Oscillation. A strong East Asian summer monsoon and an El Nino-decaying summer may also contribute to the southwesterly WVT anomalies over the TRS region.

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