Unraveling East Africa's Climate Paradox
Unraveling East Africa's Climate Paradox
复制标题
解开东非的气候悖论
DOI:
10.1002/9781119068020.ch16
复制
发表时间:
2017
影响因子:
4.9
通讯作者:
N. Vigaud
中科院分区:
文献类型:
--
作者:
B. Lyon;N. Vigaud
Several East African countries are currently facing something of a climate paradox [Lyon, 2014]. For well over a decade, the region has been experiencing an increased frequency of drought (Fig. 16.1a), the most recent and severe of these events (in 2010–2011) triggering a humanitarian crisis and prompting a major international response [FEWSNET, 2011]. This rainfall decline has led to inevitable speculation that an anthropogenic climate change signal has begun to emerge in the region. Yet, paradoxically, climate model projections show a general consensus that increasing greenhouse gasses will in fact result in East Africa’s climate becoming wetter during the current century (Fig. 16.1b) [Christensen et al., 2007; Shongwe et al., 2011]. Confounding this seeming paradox, in many parts of East Africa the rainfall seasonal cycle is bimodal, with the bulk of the recent rainfall decline occurring during the “long rains” season of March–May (MAM; other seasons denoted similarly) while the “short rains” of October–December (OND) show an upward trend over the past three decades [e.g., Liebmann et al., 2014]. These divergent outcomes highlight the need to identify the physical mechanisms associated with both the observed and projected changes in East African climate. From a physical perspective, a true paradox is of course illusory and several hypotheses can be contemplated to account for the differing trends. For example, the coupled climate models (CMIP5) used to project the future c limate may be missing, or misrepresenting, key physical processes important to East African rainfall. The future may indeed become drier and the model projections are simply wrong. Alternatively, the recent drying may be a Unraveling East Africa’s Climate Paradox
影响因子:
4.6
作者:
Bayr, Tobias;Dommenget, Dietmar;Power, Scott B.
通讯作者:
Power, Scott B.