Institute of Loess Plateau, Shanxi University, Taiyuan, 030006, Shanxi, China.
College of Natural Resources & Environment, Northwest A & F University, Yangling, 712100, Shaanxi, China.
Environ Sci Pollut Res Int. 2019 Dec;26(35):35717-35727. doi: 10.1007/s11356-019-06440-z. Epub 2019 Nov 7.
Asymmetric warming has been increasingly discussed recently, yet knowledge of this difference in warming between daytime and nighttime is still limited. Most studies of how climate warming influences the terrestrial ecosystem often ignore this asymmetric effect. We investigated the change in temperature between daytime and nighttime and analyzed the relationships between normalized difference vegetation index and the temperature in the daytime (T) and the nighttime (T) from 1982 to 2015 in temperate China. Results showed a faster increase in T (0.46 °C dec, p < 0.01) during the nighttime than in T (0.42 °C dec, p < 0.01) during the daytime, which indicated an asymmetric warming rate. The asymmetric warming during the daytime and nighttime was closely related to variations in precipitation and solar radiation. The increasing T and T were most pronounced over a large portion of the entire temperate China, and their warming trends displayed a non-uniform spatial distribution. The area with daytime warming was larger than that with nighttime warming, approximately accounting for 99.53% and 96.22% of temperate China, respectively. The area with warming enhancing vegetation greenness was larger during the day (71.16% of temperate China, p < 0.05) than at night (61.60% of temperate China, p < 0.05), and vice versa, which presented asymmetric warming effects on China's temperate vegetation. We also found clear differences in the responses of the normalized difference vegetation index among different vegetation biomes to this asymmetric warming. Averagely, T was significantly related to the NDVI of shrub, desert, broadleaf forest, needleleaf forest, and swamp (p < 0.01). However, this similar relationship appeared only between T and desert vegetation (p < 0.01). Our findings emphasized the crucial role of asymmetric warming between the daytime maxima and nighttime minima in climate change research.
近年来,非对称性增暖现象受到了越来越多的关注,然而,人们对昼夜之间增暖差异的认识仍然有限。大多数研究气候变暖如何影响陆地生态系统的研究往往忽略了这种非对称性效应。我们研究了 1982 年至 2015 年期间,中国温带地区昼夜间温差的变化,并分析了归一化植被指数与日间温度(T)和夜间温度(T)之间的关系。结果表明,夜间 T 的增长率(0.46°C/dec,p<0.01)快于日间 T 的增长率(0.42°C/dec,p<0.01),表明存在非对称性增暖速率。日间和夜间的非对称性增暖与降水和太阳辐射的变化密切相关。在中国温带地区的大部分地区,T 和 T 的增温最为显著,其增温趋势呈现出非均匀的空间分布。白天增温的区域大于夜间增温的区域,分别约占中国温带地区的 99.53%和 96.22%。白天增温使植被变绿的区域大于夜间增温使植被变绿的区域,分别占中国温带地区的 71.16%(p<0.05)和 61.60%(p<0.05),这表明非对称性增暖对中国温带植被有不同的影响。我们还发现,不同植被生物群落在应对这种非对称性增暖时,归一化植被指数的响应存在明显差异。平均而言,T 与灌木、沙漠、阔叶林、针叶林和沼泽的 NDVI 显著相关(p<0.01)。然而,这种相似的关系仅存在于 T 与沙漠植被之间(p<0.01)。我们的研究结果强调了非对称性增暖在气候变化研究中的重要作用。