干旱环境监测
榦旱環境鑑測
간한배경감측
ARID ENVIRONMENTAL MONITORING
2015年
2期
82-86
,共5页
乌鲁木齐:趋势%气候极值
烏魯木齊:趨勢%氣候極值
오로목제:추세%기후겁치
Urumqi%trend%climate extremes
基于乌鲁木齐近60年的气温、降水资料,运用Mann-Kendall和线性回归检验对气候变量序列进行了趋势和极值分析。结果表明,平均气温、平均最高气温、平均最低气温表现出增加趋势且以秋冬季的增温幅度最大。气温日较差在所有时间步长内都是缩小的,其主要原因是平均最低气温的升温幅度比最高气温大,降水量总体上增加,季节降水中以冬季增加最为明显。从气候极值变化方面看,与异常偏冷相关的极端事件如霜冻日数、冷夜日数、冷昼日数、冷日持续指数显著减少减弱;与异常偏暖相关的暖夜日数、暖昼日数则明显增多增强;降水强度、强降水量增加明显,持续干旱有所下降。
基于烏魯木齊近60年的氣溫、降水資料,運用Mann-Kendall和線性迴歸檢驗對氣候變量序列進行瞭趨勢和極值分析。結果錶明,平均氣溫、平均最高氣溫、平均最低氣溫錶現齣增加趨勢且以鞦鼕季的增溫幅度最大。氣溫日較差在所有時間步長內都是縮小的,其主要原因是平均最低氣溫的升溫幅度比最高氣溫大,降水量總體上增加,季節降水中以鼕季增加最為明顯。從氣候極值變化方麵看,與異常偏冷相關的極耑事件如霜凍日數、冷夜日數、冷晝日數、冷日持續指數顯著減少減弱;與異常偏暖相關的暖夜日數、暖晝日數則明顯增多增彊;降水彊度、彊降水量增加明顯,持續榦旱有所下降。
기우오로목제근60년적기온、강수자료,운용Mann-Kendall화선성회귀검험대기후변량서렬진행료추세화겁치분석。결과표명,평균기온、평균최고기온、평균최저기온표현출증가추세차이추동계적증온폭도최대。기온일교차재소유시간보장내도시축소적,기주요원인시평균최저기온적승온폭도비최고기온대,강수량총체상증가,계절강수중이동계증가최위명현。종기후겁치변화방면간,여이상편랭상관적겁단사건여상동일수、랭야일수、랭주일수、랭일지속지수현저감소감약;여이상편난상관적난야일수、난주일수칙명현증다증강;강수강도、강강수량증가명현,지속간한유소하강。
Abstar ct:There has been a paucity of information on trends in daily climate and climate extremes especially from developing countries.We reported the results of analysis of daily temperature( maximum and minimum) and precipitation data form Uru-mqi.Data were subject to quality control and processing into indices of climate extremes for release to the global community. Based on the temperature and precipitation data over the last 60 years,this paper analyzed trends and climate extremes using Mann-Keandall and linear regression test.The results showed that mean temperature,maximum mean temperature,minimum mean temperature indicated an increasing trend while the warming amplitudes in the autumn and winter was the largest.The main reason of the reduced diurnal temperature range in all time steps was that minimum mean temperature had a larger in-creasing temperature range than maximum mean temperature.Overall,precipitation appeared to be increased and it emerged the most obvious increasing in winter.Both temperature and precipitation in different months had different trends,but the most sig-nificant change was basically happened in January and February.The extremes ralated to low temperature such as frost days, cool nights,cool days,cold spell duration indicator,have been obviously decreased in frequency and intensity,and the extrenes ralated to high temperature such as warm nights,warm days,have been mostly increased in frequency and intensity.The simple daily intensity index and very wet day have witnessed significant upward trend and consecutive dry day have gradually drop weakened.