遞減尺度 的英文怎麼說

中文拼音 [jiǎnchǐ]
遞減尺度 英文
regressive scale
  • : Ⅰ動詞(傳送;傳遞) hand over; pass; give Ⅱ副詞(順著次序) in the proper order; successively
  • : 尺名詞[音樂] (中國民族音樂音階上的一級 樂譜上用做記音符號 參看「工尺」) a note of the scale in ...
  • : 度動詞[書面語] (推測; 估計) surmise; estimate
  • 遞減 : (一次比一次減少) decrease progressively [successively]; decrease by degrees; reduce progressively
  1. For the first few thousand feet above sea level the rate of pressure decrease is in the neighbourhood of 1 inch of pressure for each 900 to 1000 ft

    在離海面幾千英上(在拔海高數千英以下)氣壓率大約是每900到1000英下降1英寸汞柱左右。
  2. The bandwidth of a copper wire decreases exponentially with length, and hence adsl data rates drop by 10x in going from 6000 feet to 18000 feet

    答案:在銅線上頻率是隨著長以陪數,所以adsl的數據傳輸率從6000至18000是以10陪下跌。
  3. Detailed diagnoses is made on a heavy - hard rain in the northeast qinghai - xizang plateau using ncep data of 1 x 1 with 6h intervals, more complete and integrated conventional observational data and the data set of automatic meteorological stations in plateau and new generation doppler radar data and satellite images and etc. the following conclusions can be drawn : 1. the distribution of heavy - hard rain, which is characteristics of valley topography in northeast qinghai - xizang plateau is obviously effected by topography. the distribution of yearly mean precipitation and the frequencies of heavy - hard rain in this area are descending from east to west

    本文首先利用ncep時間間隔為6小時的1 1的格點資料、更全面、更為完整的常規探測資料和高原地區布設的自動氣象站資料、新一代多卜勒天氣雷達資料、衛星雲圖資料等對高原東北部地區大到暴雨的天氣、氣候特徵及大環流背景進行分析,形成對高原暴雨的整體認識,並為以後的數值模擬提供大環流背景及依據,分析中發現: 1 、高原東北部地區大到暴雨的分佈明顯受到地形影響,年降水量和大到暴雨次數自東向西呈階梯性趨勢,分別在高原東北部的外流河谷地區和四川北部地區存在大值中心。
  4. It is brought forward for the first time that in summertime the pco2 of the surface water near the changjiang estuary, whose salinity is less than 20, decreases dramatically from upwards of 800uatm to downwards of 300uatm within the range of less than half one latitude, suggesting a transformation of a strong co2 source to a co2 sink in a finite space

    首次調查得到,夏季長江口附近鹽20區域的水體極高的pco _ 2 (最高測得800 atm以上)在不到半個緯的范圍內到300 atm以下,即由一個很強的大氣co _ 2源,有限的空間范圍內變成為匯區,有著極大的梯變化。
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