Dagan Guy, Stier Philip, Watson-Parris Duncan
Atmospheric, Oceanic and Planetary Physics, Department of Physics University of Oxford Oxford UK.
Geophys Res Lett. 2019 Sep 1;46(17-18):10504-10511. doi: 10.1029/2019GL084173. Epub 2019 Sep 2.
Global mean precipitation changes due to climate change were previously shown to be relatively small and well constrained by the energy budget. However, local precipitation changes can be much more significant. In this paper we propose that for large enough scales, for which the water budget is closed (precipitation [] roughly equals evaporation []), changes in approach the small global mean value. However, for smaller scales, for which and are not necessarily equal and convergence of water vapor still plays a role, changes in could be much larger due to dynamical contributions. Using 40 years of two reanalysis data sets, 39 Coupled Model Intercomparison Project Phase 5 (CMIP5) models and additional numerical simulations, we identify the scale of transition in the importance of the different terms in the water budget to precipitation to be ~3,500-4,000 km and demonstrate its relation to the spatial scale of precipitation changes under climate change.
先前研究表明,气候变化导致的全球平均降水量变化相对较小,且受能量平衡的严格限制。然而,局部降水量变化可能要显著得多。在本文中,我们提出,对于足够大的尺度,即水分收支平衡(降水量[]大致等于蒸发量[])的尺度,[此处原文似乎有缺失内容]接近全球平均小值。然而,对于较小尺度,降水量和蒸发量不一定相等,水汽辐合仍起作用,由于动力作用,[此处原文似乎有缺失内容]的变化可能要大得多。利用40年的两个再分析数据集、39个耦合模式比较计划第五阶段(CMIP5)模式以及额外的数值模拟,我们确定了水分收支中不同项对降水重要性转变的尺度约为3500 - 4000千米,并证明了其与气候变化下降水变化空间尺度的关系。