广东水利水电
廣東水利水電
엄동수이수전
GUANGDONG WATER RESOURCES AND HYDROPOWER
2015年
7期
19-25
,共7页
气候学%暴雨%变化特征%清远
氣候學%暴雨%變化特徵%清遠
기후학%폭우%변화특정%청원
climatology%rainstorm%change characteristic%Qingyuan
利用清远地区7个气象台站1962—2012年逐日降雨量资料,统计分析了清远地区暴雨天气的气候变化特征,结果表明:清远地区年暴雨日数和暴雨量都呈弱的增加趋势,暴雨强度呈弱的减小趋势。汛期洪涝贡献率高,前汛期比后汛期更容易发生洪涝灾害。年暴雨日数、年暴雨量、暴雨强度和暴雨贡献率地域分布存在明显差异,都呈自北向南递减的趋势,但北部地区均为增加趋势,南部地区均为减少趋势。年暴雨日数和年暴雨量在1969年有一个呈显著增加趋势的突变,但持续年数短。
利用清遠地區7箇氣象檯站1962—2012年逐日降雨量資料,統計分析瞭清遠地區暴雨天氣的氣候變化特徵,結果錶明:清遠地區年暴雨日數和暴雨量都呈弱的增加趨勢,暴雨彊度呈弱的減小趨勢。汛期洪澇貢獻率高,前汛期比後汛期更容易髮生洪澇災害。年暴雨日數、年暴雨量、暴雨彊度和暴雨貢獻率地域分佈存在明顯差異,都呈自北嚮南遞減的趨勢,但北部地區均為增加趨勢,南部地區均為減少趨勢。年暴雨日數和年暴雨量在1969年有一箇呈顯著增加趨勢的突變,但持續年數短。
이용청원지구7개기상태참1962—2012년축일강우량자료,통계분석료청원지구폭우천기적기후변화특정,결과표명:청원지구년폭우일수화폭우량도정약적증가추세,폭우강도정약적감소추세。신기홍로공헌솔고,전신기비후신기경용역발생홍로재해。년폭우일수、년폭우량、폭우강도화폭우공헌솔지역분포존재명현차이,도정자북향남체감적추세,단북부지구균위증가추세,남부지구균위감소추세。년폭우일수화년폭우량재1969년유일개정현저증가추세적돌변,단지속년수단。
The climate change characteristics of rainstorm in Qingyuan have been analyzed by using the daily precipitation data of 7 weather stations from 1962 to 2012.The results show that annual rainstorm days and rainstorm amount have weak increasing trend , and rainstorm intensity has a decreasing trend .Flood contribution rate is high in flood season , and flood disaster more easily happen in pre-flood season than later flood season .Differences exist in different regions on the annual rainstorm days , annual rainstorm amount, rainstorm intensity and rainstorm contribution rate , and a decreasing trend exists from north to south;however, the whole shows that an increasing trend is in the northern region , and a decreasing trend is in the southern region .The annual rainstorm days and rainstorm amount had a significant growth but short lasting years remained in 1969.