The Tibetan Plateau has been thought to play an important role as an elevated heat source in the evolution of asian monsoon. Field measurements over the Tibetan Plateau have been conducted as the subprogram of the Global Energy and Water cycle Experiment (GEWEX). In this lecture, the summary of the field observation in the Tibetan Plateau is introduced, including some results of the diurnal/seasonal variation of surface energy fluxes.
Related web page are:
The ecology and conservation of a seasonally dry tropical forest in South America
The tangled evolutionary history of plants and fungi
From the field to the lab to integrated risk assessment of vector-borne pathogens