Publication Date

1993

Description

The subtropical regions of China, making up 28% of the total area of the country, are characterised by 3 types of ecological environment as a result of effects of the monsoon climate: Indian Ocean monsoon­dominated (dry winter-spring), Pacific Ocean monsoon-dominated (hot, dry summer), and highland transitional (moderate) types. Bach of these has specific patterns of humidity (referred to as K value) and pasture growth. The main constraints to and opportunities for grasshind farming in China's subtropics are highlighted.

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Climatic Variation in the Monsoonal Subtropics of China and its Effect on Grassland Farming

The subtropical regions of China, making up 28% of the total area of the country, are characterised by 3 types of ecological environment as a result of effects of the monsoon climate: Indian Ocean monsoon­dominated (dry winter-spring), Pacific Ocean monsoon-dominated (hot, dry summer), and highland transitional (moderate) types. Bach of these has specific patterns of humidity (referred to as K value) and pasture growth. The main constraints to and opportunities for grasshind farming in China's subtropics are highlighted.