词语大全 gauged data中文翻譯
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词语大全 gauged data中文翻譯
Project iii is the grid method by interpolating rain - gauge data to a grid element as the input of that element
方案是基于柵格單元建立的,將雨量離散到每個柵格單元作為雨量輸入。
The result agrees well with observations by paring the simulated result with the 167 tidal gauge data
通過與167個測站的4個主要分潮平均絕對偏差的比較,模擬結果與實測資料符合很好。
The theory and method on the determination of the sea level relative variation by tide gauge data is introduced in the dissertation
作者首先介紹了利用驗潮站觀測資料監測海平面相對變化的理論與方法。
Considering the effect of the crustal vertical motion , the absolute variation cannot be drawn only using the tide gauge data
由于驗潮站所在陸地垂直運動的影響,僅利用驗潮站結果,無法獲得海平面的絕對變化信息。
Project ii is modified subcatchment method by interpolating rain - gauge data to each grid , then averaging rain values over all grids within a subcatchment as the input of the ~ subcatchment
方案是在方案的基礎上,先將雨量離散到柵格單元,再將雨量劃歸到研究流域的各子流域作為雨量輸入。
First , the defmation and status of height datums is introduced and some problems on the local height datums estabpshed by the mean sea level , which is defined by the tide gauge data , are discussed . then the research progresses in recent years are analysed
首先介紹了高程基準的定義與現狀,指出了用驗潮站長期平均海平面建立局部高程基準所存在的問題;分析了當今國內外高程基準的研究現狀;進一步明確了我國高程基準現代化的必要性。
Rainfall and vertical profile of hydrometers are retrieved for land and ocean using tmi 1b11 data . the parison of retrievals of gprof v6 . 1 and v6 . 2 with ground - based radar and gauge data on land and pr data on ocean show that the gprof - v6 algorithm can retrieve rain intensity much well and indicate vertical distribution of hydrometers mainly . as far as retrieved precipitation area , it is better for convective precipitation type than stratified precipitation type
將陸地的反演結果與地基雷達資料和地面雨量計資料進行比較,海洋的反演結果結合trmmpr的降水產品進行比較,結果表明: gprof - v6算法反演的降水產品可以較好地反映降水強度并反映降水的主要垂直結構;在落區方面,對流降水反映較好,層云降水則較差;云-輻射數據集的擴充與改進可提高反演精度。
The diurnal constituents at some of the crossover points and all of the semi - diurnal constituents at all of the crossover points as well as 16 tidal gauge data are assimilated in the ocean model , this is because the assimilation of the diurnal constituents at some crossover points make the result worse . the improvement is 36 % for m2 , 54 % for s2 , 42 % for k , , 30 % for 01 pared with the results of dynamic model without assimilation . in the stratified ocean , mixing controls the intensity of the ocean current
為了克服交叉點上全日分潮精度較低的局限,文中主要將半日分潮同化進模式中,而全日分潮只在部分交叉點上進行了同化,同時同化了沿岸16個驗潮站的調和常數,同化高度計資料和沿岸資料后, m _ 2 、 s _ 2 、 k _ 1 、 o _ 1四個主要分潮的結果精度分別提高36 、 48 、 20 、 12 。
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