The quantitative comparison of contributions from vapour and temperature to midsummer precipitation in China under the influence of spring heat source over Tibet Plateau-Reference-Cited by-同舟云学术

The quantitative comparison of contributions from vapour and temperature to midsummer precipitation in China under the influence of spring heat source over Tibet Plateau

Published:2021-08-23 Issue: Volume: Page:
ISSN:0899-8418
Container-title:International Journal of Climatology
language:en
Short-container-title:Int J Climatol

Author:

Hao Jiawei¹^ORCID,Lu Er¹^ORCID

Affiliation:

1. Key Laboratory of Meteorological Disaster, Ministry of Education (KLME)/Joint International Research Laboratory of Climate and Environment change (ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC‐FEMD) Nanjing University of Information Science & Technology Nanjing China

Funder

National Basic Research Program of China

National Natural Science Foundation of China

Priority Academic Program Development of Jiangsu Higher Education Institutions

Publisher

Wiley

Subject

Atmospheric Science

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/joc.7333

Reference54 articles.

1. Preliminary research on inhomogeneous distribution of Tibetan Plateau sensible heat fluxes in spring;Bai J.Y.;Journal of Applied Meteorology Science,2003

2. The influence of soil temperature abnormal over the Tibetan Plateau in soring on summer flooding of the mid and lower reaches of the Changjiang River in 1988;Bai J.Y.;Quarterly Journal of Applied Meteorology,1999

3. Thermal field over Tibetan Plateau and Indian summer monsoon rainfall;Bansod S.D.;International Journal of Climatology,2003

4. Springtime precipitation and water vapor flux over southeastern South America;Berbery E.H.;Monthly Weather Review,2000

5. Relationships between water vapor path and precipitation over the tropical oceans;Bretherton C.S.;Journal of Climate,2004

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