O'Gorman Paul A
Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, 77 Massachusetts Avenue, Cambridge, MA 02139 USA.
Curr Clim Change Rep. 2015;1(2):49-59. doi: 10.1007/s40641-015-0009-3.
The response of precipitation extremes to climate change is considered using results from theory, modeling, and observations, with a focus on the physical factors that control the response. Observations and simulations with climate models show that precipitation extremes intensify in response to a warming climate. However, the sensitivity of precipitation extremes to warming remains uncertain when convection is important, and it may be higher in the tropics than the extratropics. Several physical contributions govern the response of precipitation extremes. The thermodynamic contribution is robust and well understood, but theoretical understanding of the microphysical and dynamical contributions is still being developed. Orographic precipitation extremes and snowfall extremes respond differently from other precipitation extremes and require particular attention. Outstanding research challenges include the influence of mesoscale convective organization, the dependence on the duration considered, and the need to better constrain the sensitivity of tropical precipitation extremes to warming.
利用理论、模型和观测结果来考量极端降水对气候变化的响应,重点关注控制该响应的物理因素。气候模型的观测和模拟表明,极端降水会随着气候变暖而加剧。然而,当对流起重要作用时,极端降水对变暖的敏感性仍不确定,且在热带地区可能比温带地区更高。有几种物理因素影响着极端降水的响应。热力学因素的影响是显著且已得到充分理解的,但对微物理和动力学因素影响的理论理解仍在发展中。地形性极端降水和降雪极端降水与其他极端降水的响应不同,需要特别关注。突出的研究挑战包括中尺度对流组织的影响、对所考虑持续时间的依赖性,以及更好地限制热带极端降水对变暖敏感性的必要性。