水利科技与经济
水利科技與經濟
수리과기여경제
2015年
4期
49-53
,共5页
麦麦提敏·库德热提%阿不都·沙拉木%热紫艳
麥麥提敏·庫德熱提%阿不都·沙拉木%熱紫豔
맥맥제민·고덕열제%아불도·사랍목%열자염
径流变化特征%降水与气温%原因分析%乌鲁木齐河上游
徑流變化特徵%降水與氣溫%原因分析%烏魯木齊河上遊
경류변화특정%강수여기온%원인분석%오로목제하상유
runoff variation characteristics%precipitation and temperature%reasons analysis%river outlet of Urumqi River
利用乌鲁木齐河1957-2009年的径流、气温、降水逐月资料,分析乌鲁木齐河上游出山口年径流变化特征及其与气候变化的关系。研究结果表明:①乌鲁木齐河上游出山口径流的年际变化相对稳定,但年内分配极不平衡,其中夏季径流量最大,约占全年的61.8%,其他各月径流量只占全年的38.2%;从汛期和枯期来看,乌鲁木齐河上游汛期和枯水期径流量相差较大;②近50年来,随着乌鲁木齐河上游流域出现明显的升温趋势,流域内降水呈减少的趋势;从径流年际变化的分析来看,随着乌鲁木齐河上游流域来水的增加,降水和气温的变化显著。
利用烏魯木齊河1957-2009年的徑流、氣溫、降水逐月資料,分析烏魯木齊河上遊齣山口年徑流變化特徵及其與氣候變化的關繫。研究結果錶明:①烏魯木齊河上遊齣山口徑流的年際變化相對穩定,但年內分配極不平衡,其中夏季徑流量最大,約佔全年的61.8%,其他各月徑流量隻佔全年的38.2%;從汛期和枯期來看,烏魯木齊河上遊汛期和枯水期徑流量相差較大;②近50年來,隨著烏魯木齊河上遊流域齣現明顯的升溫趨勢,流域內降水呈減少的趨勢;從徑流年際變化的分析來看,隨著烏魯木齊河上遊流域來水的增加,降水和氣溫的變化顯著。
이용오로목제하1957-2009년적경류、기온、강수축월자료,분석오로목제하상유출산구년경류변화특정급기여기후변화적관계。연구결과표명:①오로목제하상유출산구경류적년제변화상대은정,단년내분배겁불평형,기중하계경류량최대,약점전년적61.8%,기타각월경류량지점전년적38.2%;종신기화고기래간,오로목제하상유신기화고수기경류량상차교대;②근50년래,수착오로목제하상유류역출현명현적승온추세,류역내강수정감소적추세;종경류년제변화적분석래간,수착오로목제하상유류역래수적증가,강수화기온적변화현저。
Use the monthly average runoff , temperature and precipitation data from the upper reach of Urumqi river basin during 1957-2009 , the characteristics and reasons of the upper reach runoff change in Urumqi River basin in the recent 50 years were analyzed.Results showed that:①The an-nual variability of the upper reach runoff of Urumqi river is relatively stable.However , unbalanced distribution of seasonal runoff is distinct within a years; the runoff mainly concentrated on summer (June, July, August) and accounts for 61.8% of the annual runoff while the accumulative propor-tion of other three seasons account only for 38.2%.In terms of the flood season and dry period , the runoff between them usually has large fluctuation;②The temperature from the upper reach of Urumqi River basin has a trend of obvious increase in recent 50 years while precipitation has a trend of de-crease.From the initial analysis of the generation changes of the upper reach of the Urumqi River , we can get with the increase of run off , the precipitation and temperature of this area also changes significantly.