Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun 130102, China.
College of Forestry, Northeast Forestry University, Harbin 150040, China.
Sci Total Environ. 2017 Jan 1;575:1211-1218. doi: 10.1016/j.scitotenv.2016.09.187. Epub 2016 Sep 30.
As a fragile ecological zone, the temperate grassland region of China has experienced dramatic land use/land cover (LULC) changes due to human disturbances. So far, the impacts of LULC change on climate especially the diurnal temperature range (DTR) in this region are still not well understood. Based on the OMR (observation minus reanalysis) method, this study investigated the effects of LULC on DTR in the temperate grassland region of China. Considering the possible uncertainty of the results due to spatial resolution of the reanalysis dataset, two reanalysis datasets with different spatial resolutions were utilized. Results showed that LULC generally contributed to the decline of DTR in the temperate grassland region of China during 1980 to 2005. Due to different warming effects on monthly maximum temperature (Tmax) and minimum temperature (Tmin), grassland and forest tend to slightly decrease monthly DTR (approximately -0.053 to -0.050°C/decade and approximately -0.059 to -0.055°C/decade, respectively), while bare land has a slightly positive effect on DTR (approximately 0.018-0.021°C/decade). By contrast, cropland and urban tend to slightly decrease Tmax, obviously increase Tmin and thus result in a rapid decline of DTR (approximately -0.556 to -0.503°C/decade and approximately -0.617 to -0.612°C/decade, respectively). In the temperate grassland region of China, grassland vegetation changes due to human disturbances can have some effects on DTR mainly by changing the Tmax. Conversion from grassland to cropland could decrease the DTR by slowing down the increase of Tmax. But the conversion from grassland to bare land, as well as the reduction of grassland vegetation cover will increase Tmax, and consequently the DTR. The results suggest that grassland degradation is likely to result in daylight warming and increased DTR in the temperate grassland region of China.
作为一个生态脆弱区,中国温带草原区由于人类干扰经历了剧烈的土地利用/土地覆盖(LULC)变化。到目前为止,LULC 变化对气候的影响,特别是该地区日较差(DTR)的影响还没有得到很好的理解。本研究基于 OMR(观测与再分析差值)方法,调查了 LULC 变化对中国温带草原区 DTR 的影响。考虑到再分析数据集空间分辨率可能导致结果存在不确定性,使用了两个具有不同空间分辨率的再分析数据集。结果表明,1980 年至 2005 年期间,LULC 普遍导致中国温带草原区 DTR 下降。由于对月最高温度(Tmax)和最低温度(Tmin)的不同升温效应,草地和林地对月 DTR 有略微的降低作用(分别约为-0.053 至-0.050°C/decade 和约为-0.059 至-0.055°C/decade),而裸地对 DTR 有略微的正效应(约为 0.018-0.021°C/decade)。相比之下,耕地和城市有略微降低 Tmax、明显增加 Tmin 的趋势,导致 DTR 快速下降(分别约为-0.556 至-0.503°C/decade 和约为-0.617 至-0.612°C/decade)。在中国温带草原区,由于人类干扰导致的草地植被变化可能主要通过改变 Tmax 对 DTR 产生一定影响。草地向耕地的转化可以通过减缓 Tmax 的增加来降低 DTR。但草地向裸地的转化以及草地植被覆盖的减少,会增加 Tmax,从而导致 DTR 升高。结果表明,草地退化可能导致中国温带草原区白天变暖,DTR 增加。