/   Home   /   Newsroom   /   Research News

IAP Scientists Reveal Feedback of South Asian Summer Monsoon to Tibetan Surface Heating

Jan 19, 2016     Email"> PrintText Size

The Tibetan Plateau is an important heating source to the atmosphere, with great impacts on the weather, climate and environment systems in Asia and the Northern Hemisphere. The surface heating process of the plateau is therefore drawing attentions of the scientists and public. It’s generally believed that the Tibetan surface heating driven meridian circulation affects the onset and evolution of the South Asian summer monsoon. However, the monsoon hardly has feedback to the surface heating on the Tibetan Plateau due to the Himalayas blocking.  

More than half of the plateau surface is covered by giant mountain systems. In recent years, ZOU Han, ZHOU Libo and their colleagues in the Institute of Atmospheric Physics, Chinese Academy of Sciences have been operating atmospheric experiments in the Himalayas region, and revealed the unique surface heating process in the Tibetan mountains and the negative feedback of the South Asian summer monsoon to the surface heating.  

They found that the complex topography in the Tibetan mountains traps great amount of solar energy, and gains a high surface temperature; and that the heat energy is transferred from the surface to the free atmosphere via the near surface turbulence and local circulation with much higher efficiency than the flat regions. This surface heating process is very sensitive to the input of solar energy, i.e., the strong solar radiation increases the surface heat energy, and enhances the upward heat transfer driven by the turbulence and local circulation, and vice versa.  

“The large cloud amount at high altitudes brought by the South Asian summer monsoon circulation efficiently blocks the solar radiation input,” Dr. ZOU explained, “It lowers the surface heat energy and weakens the heat energy transferred from the surface to the free atmosphere by the near surface turbulence and local circulation, and therefore depresses the surface heating in the Tibetan mountains.” 

The findings lead to a more comprehensive understanding on the Tibetan surface heating and its interaction with the neighboring climate systems.


(Editor: CHEN Na)

Related Articles

Tibetan Plateau;precipitation;monsoon onset;Interdecadal Pacific Oscillation

Tibetan Plateau Gets Wetter and Greener in Early Summer in Recent Decades

Aug 11, 2017

The change of water supplies over the TP has long been a “hotspot” of climate change research. Recently, a new study conducted by Dr. ZHANG Wenxia, Prof. ZHOU Tianjun and Dr. ZHANG Lixia from Institute of Atmospheric Physics, Chinese Academy of Sciences shows that the T...

Tibetan Plateau;tectonic plate;Asian plate

Mystery of the Tibetan Plateau Solved: Study Finds the Strength of Tectonic Plates Caused its Unique Shape

Jul 25, 2017

Researchers have discovered the Tibetan Plateau's shape, which dwarfs other mountain ranges in height and breadth, may be controlled mostly by the strength of the tectonic plates whose collision prompted its uplift. While most mountain ranges appear like narrow scars of r...

Contact Us

Copyright © 2002 - Chinese Academy of Sciences