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      氣候變化研究進(jìn)展 ?? 2010, Vol. 6 ?? Issue (06): 405-410.

      ? 氣候系統(tǒng)變化 ? 上一篇    下一篇

      典型相關(guān)分析方法對(duì)21世紀(jì)江淮流域極端降水的預(yù)估試驗(yàn)

      崔妍,江志紅,陳威霖   

      1. 南京信息工程大學(xué)
      • 收稿日期:2010-03-12 修回日期:2010-04-13 出版日期:2010-11-30 發(fā)布日期:2010-12-10
      • 通訊作者: 江志紅 E-mail:zhjiang@nuist.edu.cn

      Projection of Extreme Precipitation Events in the 21st Century in the Changjiang-Huaihe River Valley Based on Canonical Correlation Analysis

      • Received:2010-03-12 Revised:2010-04-13 Online:2010-11-30 Published:2010-12-10
      • Contact: Jang Zhihong E-mail:zhjiang@nuist.edu.cn

      摘要: 利用1961—1990年江淮流域逐日降水資料、NCEP/NCAR再分析資料和HadCM3 SRES A1B情景下模式預(yù)估資料,采用典型相關(guān)分析統(tǒng)計(jì)降尺度方法,評(píng)估降尺度模型對(duì)當(dāng)前極端降水指數(shù)的模擬能力,并對(duì)21世紀(jì)中期和末期的極端降水變化進(jìn)行預(yù)估。結(jié)果表明:通過降尺度能夠有效改善HadCM3對(duì)區(qū)域氣候特征的模擬能力,極端降水指數(shù)氣候平均態(tài)相對(duì)誤差降低了30%~100%,但降尺度結(jié)果仍然在冬季存在濕偏差、夏季存在干偏差;在SRES A1B排放情景下,該區(qū)域大部分站點(diǎn)的極端強(qiáng)降水事件將增多,強(qiáng)度增大,極端強(qiáng)降水指數(shù)的變化幅度高于平均降水指數(shù),且夏季增幅高于冬季;冬季極端降水貢獻(xiàn)率(R95t)在21世紀(jì)中期和末期的平均增幅分別為14%和25%,夏季則分別增加24%和32%。

      關(guān)鍵詞: 統(tǒng)計(jì)降尺度, 典型相關(guān)分析, 極端降水, 預(yù)估, statistical downscaling, canonical correlation analysis, extreme precipitation, projection

      Abstract: Based on the observed daily precipitation data at 26 meteorological stations in the Changjiang-Huaihe River valley, and the NCEP/NCAR reanalysis data from 1961 to 1990 as well as the climate projections in middle and late 21st century by the HadCM3 model under the IPCC SRES A1B, the simulation capabilities of the statistical downscaling approach for extreme precipitation indices of the current climate have been assessed by applying canonical correlation analysis (CCA). In addition, future extreme precipitation indices in middle and late 21st century have been projected. The results show that the modeling capacity of the HadCM3 for regional climate characteristics can be effectively improved by the downscaling approach, with reducing the relative error of the climatological average state of extreme precipitation indices by 30% -100%. However, the downscaling results are still wetter in winter and dryer in summer than observations. Under the SRES A1B, frequency and intensity of extreme precipitation events are projected to increase, and the estimated increasing rate is higher for extreme precipitation index than for average one, and in summer than in winter. Fractions of extreme precipitation in middle/late 21st century are expected to increase by 14% / 25% in winter, and by 24% / 32% in summer, respectively.

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