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Elevation, particularly in the Andes, is another important climatic control.
Lucht, W. et al. Climatic control of the high-latitude vegetation greening trend and Pinatubo effect.
The inset graph shows the total proportional areas experiencing significant trends in the three climatic control factors.
For example, climatic control of local vegetation zones was often found insufficient to explain vegetation changes; on the contrary, soil patterns and geologic history quite override climatic control in many localities.
How to characterize, quantitatively, this climatic control on the perennial stream distributions is a pertinent question for further hydro-geomorphological research.
The observed changes in climatic control factors predominantly favor increasing ET, consistent with the finding of rising global land ET over the same period.
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Our best model contained just two variables representing soil moisture and climate, suggesting that soil and climatic controls over agricultural suitability can be effectively represented by the interactive effects of the long-term mean annual frequency of wet degree days in the top soil layers and the long-term mean annual number of days with maximum temperature greater than 34 °C.
In some regions, severe climatic controls cause a particular process agent to become preeminent.
West, A. J., Galy, A. & Bickle, M. Tectonic and climatic controls on silicate weathering.
Climatic controls on these cycles are incompletely known.
Yang, Y. et al. Edaphic rather than climatic controls over 13C enrichment between soil and vegetation in alpine grasslands on the Tibetan Plateau.
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