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Climate in the Mongolian steppe during 2000-2010.

Climate in the Mongolian steppe during 2000-2010.

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Spatial patterns of herbaceous biodiversity in Mongolia steppe were examined and explained with biotic and abiotic factors including climate, livestock grazing, and fire disturbance. Vegetation data were collected from 63 sites across different steppe types (i.e., semi-desert, typical, and forb steppes) in 2012 and 2013. Three categorical (three st...

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Context 1
... the latitudinal gradients from south to north, precipitation increases and air temperature decreases, and steppe type changes from semi-desert to forb-steppe types. Such distinct climatic gradients were identified across the weather stations in our study area (Table 1). Generally, distinct biome-specific climate gradient in our study region can be distinguished as: hot (mean annual temperature 2.6 °C) and dry (mean annual precipitation 132 mm y −1 ) semi-desert steppe, cool (0.40 °C) and wet (284 mm y −1 ) forbsteppe, and intermediate temperature (1.39 °C) and precipitation (201 mm y −1 ) of typical steppe (Table 1). ...
Context 2
... distinct climatic gradients were identified across the weather stations in our study area (Table 1). Generally, distinct biome-specific climate gradient in our study region can be distinguished as: hot (mean annual temperature 2.6 °C) and dry (mean annual precipitation 132 mm y −1 ) semi-desert steppe, cool (0.40 °C) and wet (284 mm y −1 ) forbsteppe, and intermediate temperature (1.39 °C) and precipitation (201 mm y −1 ) of typical steppe (Table 1). ...
Context 3
... biotic and abiotic factors were collected for explaining spatial biodiversity pattern. Monthly climatic data (year 2001 to 2010) from 10 meteorological stations (Table 1, triangles in Fig. 1a) were collected from the Mongolia Institute of Meteorology, Hydrology, and Environment for the study regions. We assumed that site weather could be represented by the climatic data from the nearest meteorological station if they were less than 50 km from each other. ...

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... Major mountain ranges (e.g., the Altai and Sayan Range in the northwest, the Khangai Range in the central region, and the Great Hingan Range in the east) intercept moisture, resulting in rain shadow regions in the west, south, and southeast [21]. Precipitation decreases gradually from the northern to the southern territory, where forest steppe, typical steppe, desert steppe, and desert occur in turn; vegetation production and biodiversity are positively correlated with precipitation [3,27,28]. ...
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