Climatic response to changes in vegetation in the Northwest Hetao Plain as simulated by the WRF model

Authors

  • Entao Yu,

    Corresponding author
    1. Nansen-Zhu International Research Center, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China
    2. Climate Change Research Center, Chinese Academy of Sciences, Beijing, China
    3. Graduate School of the Chinese Academy of Sciences, Beijing, China
    • Nansen-Zhu International Research Center, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China.
    Search for more papers by this author
  • Huijun Wang,

    1. Nansen-Zhu International Research Center, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China
    2. Climate Change Research Center, Chinese Academy of Sciences, Beijing, China
    Search for more papers by this author
  • Jianqi Sun,

    1. Nansen-Zhu International Research Center, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China
    Search for more papers by this author
  • Yongqi Gao

    1. Nansen-Zhu International Research Center, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China
    2. Nansen Environmental and Remote Sensing Center, Bjerknes Centre for Climate Research, Bergen, Norway
    Search for more papers by this author

Abstract

Considering the ‘Green Great Wall’ project and future climate change, the vegetation in the Northwest Hetao Plain (NWHP) of China is expected to undergo considerable changes. In this study, the climatic response to prescribed changes in vegetation is investigated using the Weather Research and Forecasting model. When the vegetation is changed from ‘bare or sparsely vegetated’ category to ‘grassland’ in the NWHP, the climate shows both local and remote responses. Locally, the temperature increases in the winter but decreases in the summer. The precipitation level increases substantially in the summer while increases slightly in the winter, which is mainly caused by the increase in the amount of water-vapour and circulation adjustment. Additionally, atmospheric circulation anomalies also lead to remote circulation responses, including a decrease in precipitation over Central North China and an increase in precipitation over Central and South China. The results of this study bring to light the local and remote climatic responses to changes in vegetation in the NWHP using a state-of-the-art regional climate model. Copyright © 2012 Royal Meteorological Society

Ancillary