气象与环境学报
氣象與環境學報
기상여배경학보
JOURNAL OF METEOROLOGY AND ENVIRONMENT
2014年
4期
34-41
,共8页
崔妍%周晓宇%赵春雨%龚强%王颖%李倩%敖雪%房一禾%张海娜
崔妍%週曉宇%趙春雨%龔彊%王穎%李倩%敖雪%房一禾%張海娜
최연%주효우%조춘우%공강%왕영%리천%오설%방일화%장해나
全球气候模式%多模式集合平均%降水%模式评估%情景预估
全毬氣候模式%多模式集閤平均%降水%模式評估%情景預估
전구기후모식%다모식집합평균%강수%모식평고%정경예고
Global climate model%Multi-model ensemble mean%Precipitation%Model evaluation%Scenarios projec-tions
利用IPCC AR4中5个全球气候模式数据集和中国东北三省162个站降水实测资料,评估5个全球气候模式和多模式集合平均对中国东北三省降水的模拟能力,并对SRES B 1、A1 B 和A2三种排放情景下东北三省未来降水的变化进行预估。结果表明:全球气候模式能较好模拟东北三省降水的月变化,但存在系统性湿偏差;多模式集合平均能较好模拟东北三省年降水量的空间分布,但模拟中心偏北,强度略强,模式对东北三省夏季降水的模拟效果优于冬季降水。预估结果表明,三种排放情景下21世纪中前期和末期东北三省降水均将增多,21世纪末期增幅高于21世纪中前期,冬季增幅高于其他季节;就排放情景而言,SRES A1 B和A2排放情景增幅相当,高于B 1排放情景增幅;不同排放情景下东北三省降水量增幅分布呈较一致变化,A2排放情景下,增幅最显著的辽宁环渤海地区年降水量在21世纪中前期将增加7%以上,21世纪末期将增加16%。
利用IPCC AR4中5箇全毬氣候模式數據集和中國東北三省162箇站降水實測資料,評估5箇全毬氣候模式和多模式集閤平均對中國東北三省降水的模擬能力,併對SRES B 1、A1 B 和A2三種排放情景下東北三省未來降水的變化進行預估。結果錶明:全毬氣候模式能較好模擬東北三省降水的月變化,但存在繫統性濕偏差;多模式集閤平均能較好模擬東北三省年降水量的空間分佈,但模擬中心偏北,彊度略彊,模式對東北三省夏季降水的模擬效果優于鼕季降水。預估結果錶明,三種排放情景下21世紀中前期和末期東北三省降水均將增多,21世紀末期增幅高于21世紀中前期,鼕季增幅高于其他季節;就排放情景而言,SRES A1 B和A2排放情景增幅相噹,高于B 1排放情景增幅;不同排放情景下東北三省降水量增幅分佈呈較一緻變化,A2排放情景下,增幅最顯著的遼寧環渤海地區年降水量在21世紀中前期將增加7%以上,21世紀末期將增加16%。
이용IPCC AR4중5개전구기후모식수거집화중국동북삼성162개참강수실측자료,평고5개전구기후모식화다모식집합평균대중국동북삼성강수적모의능력,병대SRES B 1、A1 B 화A2삼충배방정경하동북삼성미래강수적변화진행예고。결과표명:전구기후모식능교호모의동북삼성강수적월변화,단존재계통성습편차;다모식집합평균능교호모의동북삼성년강수량적공간분포,단모의중심편북,강도략강,모식대동북삼성하계강수적모의효과우우동계강수。예고결과표명,삼충배방정경하21세기중전기화말기동북삼성강수균장증다,21세기말기증폭고우21세기중전기,동계증폭고우기타계절;취배방정경이언,SRES A1 B화A2배방정경증폭상당,고우B 1배방정경증폭;불동배방정경하동북삼성강수량증폭분포정교일치변화,A2배방정경하,증폭최현저적료녕배발해지구년강수량재21세기중전기장증가7%이상,21세기말기장증가16%。
Based on five global climate datasets from IPCC AR4 and the observational precipitation data at 162 me-teorological stations in the Northeast China,precipitation simulated by five global climate models and the multi-model ensemble (MME)was evaluated.Precipitation change was predicted and assessed under three emission sce-narios,i.e.SRES B1,A1B and A2.The results show that monthly precipitation could be well simulated by the global climate model in the Northeast China,while simulated values are systematically wetter than observed val-ues.The MME could well simulate spatial distributions of precipitation,while simulated center lies to the north of its observed position and simulated precipitation intensity is stronger than observed values.Also,the simulated pre-cipitation using this model is more accurate in summer than in winter in the Northeast China.According to the pro-jection,precipitation could increase in the 2 1 st century under three emission scenarios.Increasing amplitude of pre-cipitation is higher in the later 2 1 st century than in the early and middle 2 1 st century,so is in winter than in other three seasons.For three emission scenarios,increasing amplitude of precipitation under SRES A2 are as much as that under SRES A1B,while both are more than that under SRES B1.Distributions of precipitation are almost simi-lar in all scenarios.Increasing amplitude of precipitation is the largest around the Bohai Sea region,and it will in-crease by 7% in the early and middle of 21st century and 16% in the later of 21st century under SRES A2.