Strong control of Southern Ocean cloud reflectivity by ice-nucleating particles
Strong control of Southern Ocean cloud reflectivity by ice-nucleating particles
复制标题
冰核粒子对南大洋云反射率的强烈控制
DOI:
--
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发表时间:
2018
影响因子:
11.1
通讯作者:
K. Carslaw
中科院分区:
文献类型:
--
作者:
J. Vergara;A. Miltenberger;K. Furtado;D. Grosvenor;B. Shipway;A. Hill;J. Wilkinson;P. Field;B. Murray;K. Carslaw
Significance Simulated clouds over the Southern Ocean reflect too little solar radiation compared with observations, which results in errors in simulated surface temperatures and in many other important features of the climate system. Our results show that the radiative properties of the most biased types of clouds in cyclonic systems are highly sensitive to the concentration of ice-nucleating particles. The uniquely low concentrations of ice-nucleating particles in this remote marine environment strongly inhibit precipitation and allow much brighter clouds to be sustained. Large biases in climate model simulations of cloud radiative properties over the Southern Ocean cause large errors in modeled sea surface temperatures, atmospheric circulation, and climate sensitivity. Here, we combine cloud-resolving model simulations with estimates of the concentration of ice-nucleating particles in this region to show that our simulated Southern Ocean clouds reflect far more radiation than predicted by global models, in agreement with satellite observations. Specifically, we show that the clouds that are most sensitive to the concentration of ice-nucleating particles are low-level mixed-phase clouds in the cold sectors of extratropical cyclones, which have previously been identified as a main contributor to the Southern Ocean radiation bias. The very low ice-nucleating particle concentrations that prevail over the Southern Ocean strongly suppress cloud droplet freezing, reduce precipitation, and enhance cloud reflectivity. The results help explain why a strong radiation bias occurs mainly in this remote region away from major sources of ice-nucleating particles. The results present a substantial challenge to climate models to be able to simulate realistic ice-nucleating particle concentrations and their effects under specific meteorological conditions.
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影响因子:
4.6
作者:
Hawcroft, Matt;Haywood, Jim M.;Stephens, Graeme
通讯作者:
Stephens, Graeme
影响因子:
5.1
作者:
Mann, G. W.;Carslaw, K. S.;Johnson, C. E.
通讯作者:
Johnson, C. E.
影响因子:
6.3
作者:
DeMott, P. J.;Prenni, A. J.;Kreidenweis, S. M.
通讯作者:
Kreidenweis, S. M.
DOI:
10.5194/gmd-2016-194-supplement
发表时间:
2017
期刊:
--
影响因子:
--
作者:
D. Walters;I. Boutle;M. Brooks;T. Melvin;R. Stratton;S. Vosper;H. Wells;K. Williams;N. Wood
通讯作者:
D. Walters;I. Boutle;M. Brooks;T. Melvin;R. Stratton;S. Vosper;H. Wells;K. Williams;N. Wood
影响因子:
6.3
作者:
Grosvenor D
通讯作者:
Grosvenor D