气候与环境研究
氣候與環境研究
기후여배경연구
CLIMATIC AND ENVIRONMENTAL RESEARCH
2014年
3期
265-277
,共13页
赵树云%智协飞%张华%王志立%王在志
趙樹雲%智協飛%張華%王誌立%王在誌
조수운%지협비%장화%왕지립%왕재지
气溶胶%BCC_AGCM2.0.1_CAM耦合模式系统%模式评估
氣溶膠%BCC_AGCM2.0.1_CAM耦閤模式繫統%模式評估
기용효%BCC_AGCM2.0.1_CAM우합모식계통%모식평고
Aerosol%BCC_AGCM2.0.1_CAM coupled model system%Assessment of model
本文讨论了国家气候中心第二代大气环流模式BCC_AGCM2.0.1和加拿大气溶胶理化模式CAM所组成的耦合模式系统对5种典型气溶胶(硫酸盐、黑碳、有机碳、沙尘和海盐)和气候要素的模拟效果。结果表明,耦合系统对5种典型气溶胶的模拟总体上比较合理,尤其是对硫酸盐、沙尘和海盐的模拟比BCC_AGCM2.0.1原有的月平均气溶胶资料有很大的改进。耦合系统模拟的全球平均气候态参量与观测/再分析资料比较一致,在总云量、陆地表面温度和降水等方面要略优于原月平均气溶胶资料的模拟结果。耦合系统对沙尘和海盐气溶胶模拟的改进使得撒哈拉沙漠和南半球中纬度海洋大气顶净太阳辐射的模拟也有所改进,而这将直接影响地表温度尤其是陆地表面温度。而不同气溶胶方案在赤道海洋上引起的云反馈不仅引起辐射的改变,还将对降水产生明显影响。
本文討論瞭國傢氣候中心第二代大氣環流模式BCC_AGCM2.0.1和加拿大氣溶膠理化模式CAM所組成的耦閤模式繫統對5種典型氣溶膠(硫痠鹽、黑碳、有機碳、沙塵和海鹽)和氣候要素的模擬效果。結果錶明,耦閤繫統對5種典型氣溶膠的模擬總體上比較閤理,尤其是對硫痠鹽、沙塵和海鹽的模擬比BCC_AGCM2.0.1原有的月平均氣溶膠資料有很大的改進。耦閤繫統模擬的全毬平均氣候態參量與觀測/再分析資料比較一緻,在總雲量、陸地錶麵溫度和降水等方麵要略優于原月平均氣溶膠資料的模擬結果。耦閤繫統對沙塵和海鹽氣溶膠模擬的改進使得撒哈拉沙漠和南半毬中緯度海洋大氣頂淨太暘輻射的模擬也有所改進,而這將直接影響地錶溫度尤其是陸地錶麵溫度。而不同氣溶膠方案在赤道海洋上引起的雲反饋不僅引起輻射的改變,還將對降水產生明顯影響。
본문토론료국가기후중심제이대대기배류모식BCC_AGCM2.0.1화가나대기용효이화모식CAM소조성적우합모식계통대5충전형기용효(류산염、흑탄、유궤탄、사진화해염)화기후요소적모의효과。결과표명,우합계통대5충전형기용효적모의총체상비교합리,우기시대류산염、사진화해염적모의비BCC_AGCM2.0.1원유적월평균기용효자료유흔대적개진。우합계통모의적전구평균기후태삼량여관측/재분석자료비교일치,재총운량、륙지표면온도화강수등방면요략우우원월평균기용효자료적모의결과。우합계통대사진화해염기용효모의적개진사득살합랍사막화남반구중위도해양대기정정태양복사적모의야유소개진,이저장직접영향지표온도우기시륙지표면온도。이불동기용효방안재적도해양상인기적운반궤불부인기복사적개변,환장대강수산생명현영향。
Using the coupled model system of the second generation Global Circulation Model of the National Climate Center (BCC_AGCM2.0.1) and Canadian Aerosol Model (CAM), the simulation of five typical aerosols (sulfate, black carbon, organic carbon, soil dust, and sea salt) and possible effects on the modeled climate are discussed in this paper. The results show that in general, the coupled system simulates the five aerosols reasonably well, and there are obvious improvements in sulfate, dust, and sea salt aerosols compared to the original monthly mean aerosol data used in BCC_AGCM2.0.1. The climatic statistics simulated by the coupled system mainly agree well with observational/reanalyzed data, and are a little better than the monthly mean aerosol data in terms of the total cloud amount, land surface temperature, and precipitation rate. The enhanced representation of dust and sea salt improves the simulation of net solar radiation at the top of the atmosphere in the Sahara Desert and mid-latitude ocean in the Southern Hemisphere and also affects the land surface temperature. The cloud feedback above the tropical ocean caused by the change in aerosol scheme not only alters radiation but also markedly influences precipitation.