The Climate of Little Ice Age Maximum in China;

A DISCUSSION ON THE VEGETATION TYPES DURING LGM TIME IN SOUTH CHINA;

With the effect of climatic change and sea level fluctuating, the channel has sway many times from south to north or from north to south since the last glaciation maximum, but its general deflection is to south.

Simulation of hydrological cycle changes over China during LGM;

MM5 SIMULATIONS OF THE CHINA REGIONAL CLIMATE OF THE LGM Ⅱ:INFLUENCES OF CHANGES OF LAND AREA,VEGETATION,AND LARGE-SCALE CIRCULATION BACKGROUND;

MM5 SIMULATIONS OF THE CHINA REGIONAL CLIMATE OF THE LGM Ⅰ:INFLUENCES OF CO_2 AND EARTH ORBIT CHANGES;

Newly-Studies on Global Continental Climate and Terrestrial Yegetation during the LGM;

There has been a big change of the sea level and seabed water temperature since the Last Glacial Maximum (LGM) in southern South China Sea.

In this article,Milkov and Sassen s model is selected to calculate the thickness of the gas hydrate stable zone (GHSZ) and the amount of gas hydrate in the Xisha Trough at present and at the last glacial maximum (LGM),respectively,and the effects of the changes in the bottom water temperature and the sea level on these were also discussed.