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What is the necessary temperature for monsoon type vegetation? 

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This change in the vegetation scenario implies that a warm and relatively more humid climate prevailed with timely arrival of the more active SW monsoon.
Our findings suggest that although precipitation plays a promoting role, temperature is still the dominant factor in vegetation phenological period at high latitudes.
Vegetation changes associated with monsoon enhancement and high-latitude summer warming are consistent with palaeoenvironmental observations, but the simulated sh...
There appears to be only episodic and localized favorable impacts of vegetation variations on the skill of precipitation and temperature simulatio...
During the rainy season the CBL temperature is more strongly associated with upper tropospheric temperatures, which are likely modulated by large-scale circulation, than with the Sahelian vegetation.
In the west and east, vegetation variability is found to be driven predominantly by temperature, with the impact of precipitation being of secondary importance.
The comparison analysis for the monsoon region, the non-monsoon region and the MBZ suggests that the response of vegetation growth to climate change is relatively sensitive in the MBZ.
Our analyses of vegetation spatial patterns at varying geographical scales suggest that an area extent of ˜200 m is optimal for examining the vegetation–temperature relationship.
The study finds that a good monsoon helps in maintaining vegetation health during following seasons.

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