There are few reference values for crop coefficients for natural grassland in FAO Irrigation and Drainage papers. The aim of this paper was to define crop coefficients under different water conditions for typical steppe vegeation in Inner Mongolia, based on actual observation data and statistical analysis, so as to accurately calculate the water demand and actual evapotranspiration of plant community in Inner Mongolia
The crop coefficient (Kc) is widely used for operational estimation of actual evapotranspiration (ET...
The Xilingol grassland covers the region bounded by 41’09”–45’31” N and 111’14”–118’25” E. It is rep...
The magnitude and seasonal dynamics of evapotranspiration (ET) for a steppe in central Mongolia was ...
There are few reference values for crop coefficients for natural grassland in FAO Irrigation and Dra...
The Xilingol Grassland in Northern China is the largest grassland ecosystem of Inner Mongolia and pl...
tThis study aimed at assessing the soil water balance, groundwater contribution, crop transpiration ...
Since the late 1990s China has promoted the "Conversion of Cropland to Forest and Grassland Pro...
This study applied grassland related multi-index and assessed the effects of climate change by inves...
The objectives of this study were to determine the characteristics of water consumption of seven for...
Precipitation, evapotranspiration (ET), and soil moisture are the key controls for the productivity ...
The main purpose of this paper was to evaluate whether or not the dual crop coefficient (DCC) method...
Water availability is a key biophysical factor determining agricultural production potential. The FA...
23 Pags.- 7 Figs. The definitive version is available at: https://onlinelibrary.wiley.com/journal/1...
The Xilingol grassland covers the region bounded by 41’09”–45’31” N and 111’14”–118’25” E. It is rep...
The crop coefficient (Kc) is widely used for operational estimation of actual evapotranspiration (ET...
The crop coefficient (Kc) is widely used for operational estimation of actual evapotranspiration (ET...
The Xilingol grassland covers the region bounded by 41’09”–45’31” N and 111’14”–118’25” E. It is rep...
The magnitude and seasonal dynamics of evapotranspiration (ET) for a steppe in central Mongolia was ...
There are few reference values for crop coefficients for natural grassland in FAO Irrigation and Dra...
The Xilingol Grassland in Northern China is the largest grassland ecosystem of Inner Mongolia and pl...
tThis study aimed at assessing the soil water balance, groundwater contribution, crop transpiration ...
Since the late 1990s China has promoted the "Conversion of Cropland to Forest and Grassland Pro...
This study applied grassland related multi-index and assessed the effects of climate change by inves...
The objectives of this study were to determine the characteristics of water consumption of seven for...
Precipitation, evapotranspiration (ET), and soil moisture are the key controls for the productivity ...
The main purpose of this paper was to evaluate whether or not the dual crop coefficient (DCC) method...
Water availability is a key biophysical factor determining agricultural production potential. The FA...
23 Pags.- 7 Figs. The definitive version is available at: https://onlinelibrary.wiley.com/journal/1...
The Xilingol grassland covers the region bounded by 41’09”–45’31” N and 111’14”–118’25” E. It is rep...
The crop coefficient (Kc) is widely used for operational estimation of actual evapotranspiration (ET...
The crop coefficient (Kc) is widely used for operational estimation of actual evapotranspiration (ET...
The Xilingol grassland covers the region bounded by 41’09”–45’31” N and 111’14”–118’25” E. It is rep...
The magnitude and seasonal dynamics of evapotranspiration (ET) for a steppe in central Mongolia was ...
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