Low Antarctic continental climate sensitivity due to high ice sheet orography
Low Antarctic continental climate sensitivity due to high ice sheet orography
复制标题
由于冰盖地形较高,南极大陆气候敏感性较低
DOI:
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发表时间:
2020
影响因子:
9
通讯作者:
L. Polvani
中科院分区:
文献类型:
--
作者:
Hansi K. A. Singh;L. Polvani
The Antarctic continent has not warmed in the last seven decades, despite a monotonic increase in the atmospheric concentration of greenhouse gases. In this paper, we investigate whether the high orography of the Antarctic ice sheet (AIS) has helped delay warming over the continent. To that end, we contrast the Antarctic climate response to CO 2 -doubling with present-day orography to the response with a flattened AIS. To corroborate our findings, we perform this exercise with two different climate models. We find that, with a flattened AIS, CO 2 -doubling induces more latent heat transport toward the Antarctic continent, greater moisture convergence over the continent and, as a result, more surface-amplified condensational heating. Greater moisture convergence over the continent is made possible by flattening of moist isentropic surfaces, which decreases humidity gradients along the trajectories on which extratropical poleward moisture transport predominantly occurs, thereby enabling more moisture to reach the pole. Furthermore, the polar meridional cell disappears when the AIS is flattened, permitting greater CO 2 -forced warm temperature advection toward the Antarctic continent. Our results suggest that the high elevation of the present AIS plays a significant role in decreasing the susceptibility of the Antarctic continent to CO 2 -forced warming.
影响因子:
5.2
作者:
Vargas Zeppetello, L. R.;Donohoe, A.;Battisti, D. S.
通讯作者:
Battisti, D. S.
DOI:
10.1073/pnas.1519132113
发表时间:
2016-02-09
影响因子:
11.1
作者:
Rietbroek, Roelof;Brunnabend, Sandra-Esther;Dahle, Christoph
通讯作者:
Dahle, Christoph