河海大学学报(自然科学版)
河海大學學報(自然科學版)
하해대학학보(자연과학판)
JOURNAL OF HOHAI UNIVERSITY (NATURAL SCIENCES)
2014年
3期
189-194
,共6页
王皓%罗静%叶金印%李致家
王皓%囉靜%葉金印%李緻傢
왕호%라정%협금인%리치가
CMORPH融合降水产品%面雨量估算%网格算术平均法%泰森多边形法
CMORPH融閤降水產品%麵雨量估算%網格算術平均法%泰森多邊形法
CMORPH융합강수산품%면우량고산%망격산술평균법%태삼다변형법
CMORPH-Gauge merged data%area rainfall estimation%grid arithmetic average method%Thiessen polygon method
基于CMORPH融合降水产品与地面观测雨量资料,分别采用网格算术平均法与泰森多边形法估算淮河流域15个子单元2008-2011年汛期(6-9月)逐日面雨量,并对2种面雨量估算结果进行对比统计分析。结果表明:15个子单元2种面雨量估算结果具有系统性差异,两者之间存在显著线性关系;逐日面雨量估算结果也存在系统性差异,利用地面观测雨量资料估算的面雨量普遍大于利用CMORPH融合降水产品的估算结果;2种面雨量估算结果在降水量级上有很好的对应关系,各降水量级完全对应的总体比例为78.8%,相差1个量级的比例为20.5%,其中小雨量级完全对应的比例高达91.4%。
基于CMORPH融閤降水產品與地麵觀測雨量資料,分彆採用網格算術平均法與泰森多邊形法估算淮河流域15箇子單元2008-2011年汛期(6-9月)逐日麵雨量,併對2種麵雨量估算結果進行對比統計分析。結果錶明:15箇子單元2種麵雨量估算結果具有繫統性差異,兩者之間存在顯著線性關繫;逐日麵雨量估算結果也存在繫統性差異,利用地麵觀測雨量資料估算的麵雨量普遍大于利用CMORPH融閤降水產品的估算結果;2種麵雨量估算結果在降水量級上有很好的對應關繫,各降水量級完全對應的總體比例為78.8%,相差1箇量級的比例為20.5%,其中小雨量級完全對應的比例高達91.4%。
기우CMORPH융합강수산품여지면관측우량자료,분별채용망격산술평균법여태삼다변형법고산회하류역15개자단원2008-2011년신기(6-9월)축일면우량,병대2충면우량고산결과진행대비통계분석。결과표명:15개자단원2충면우량고산결과구유계통성차이,량자지간존재현저선성관계;축일면우량고산결과야존재계통성차이,이용지면관측우량자료고산적면우량보편대우이용CMORPH융합강수산품적고산결과;2충면우량고산결과재강수량급상유흔호적대응관계,각강수량급완전대응적총체비례위78.8%,상차1개량급적비례위20.5%,기중소우량급완전대응적비례고체91.4%。
Based on the CMORPH-Gauge merged data and observed rain gauge data, the daily area rainfall of 15 sub-catchments in the Huaihe River Basin was calculated during flood seasons ( June to September) from 2008 to 2011, using the Thiessen polygon method and the grid arithmetic average method. Comparative statistical analysis was conducted on the results of the two methods. The results show that the two sets of area rainfall of the 15 sub-catchments exhibited systematic differences and a significant linear correlation. The daily area rainfall also showed systematic difference. The area rainfall based on rain gauge data was generally greater than that based on the CMORPH-Gauge merged data. There was a strong correspondence for the magnitude between the two sets of area rainfall. The overall correspondence ratio was 78. 8%, with the ratio of rainfall values that differed by an order of magnitude being 20 . 5%. The correspondence ratio for the light-rainfall magnitude reached 91 . 4%.