雨量分佈情況 的英文怎麼說
中文拼音 [yǔliángfēnbùqíngkuàng]
雨量分佈情況
英文
rainfall regime- 雨 : 雨名詞(從雲層中降向地面的水) rain
- 量 : 量動1. (度量) measure 2. (估量) estimate; size up
- 分 : 分Ⅰ名詞1. (成分) component 2. (職責和權利的限度) what is within one's duty or rights Ⅱ同 「份」Ⅲ動詞[書面語] (料想) judge
- 情 : 名詞1 (感情) feeling; affection; sentiment 2 (情分; 情面) favour; kindness; sensibilities; fe...
- 況 : Ⅰ名詞1 (情形) condition; situation 2 (姓氏) a surname Ⅱ動詞(比方) compare Ⅲ連詞[書面語] (...
- 雨量 : rainfall; hyetal
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The precipitation frequencies is analysed according to 1956 ~ 2000 years of rainfall record series in baoding area. the features of distribution of rainfall are detailed evaluated. firstly, the distribution of monthly precipitation is not even. for instance. the annual rainfall amount is about 548mm in whole year, about 80 % of them in summer season. secondly, yearly variation of rainfall is greater. thirdly, the abundant years usually are followed by short years, but the important changes have taken place in the last decades. before 70 ' s the abundant years took the dominant position, from the 70 ' s to the middle of 80 ' s the short years took place more frequently than ever. after the later of 80 ' s, the short years hold the main position. the above knowledge is instructive for guiding the rainwater resources effective utilization
本文利用1956 2000年保定市的長系列降雨資料,對保定市降水量進行了頻率分析、年內變化分析和多年變化分析,明確了保定市降水量年內、年際間的變化情況:保定市降水量年內分配不均,汛期( 6 - 9月)占年降水量的81 。保定市降水量年際間變化大,豐水年和枯水年交替發生, 70年代以前以豐水年段為主; 70年代到80年代前期降水量豐枯交替頻繁,總的接近於枯水年段; 80年代後期至今以枯水年段為主。這種降水分佈規律對農業生產雨水資源的高效利用具有重要的指導意義。Readings from a network of more than 70 automatic rain - gauges covering the whole of the special administrative region are telemetered to the observatory headquarters to provide real - time information essential for assessing the likelihood of flooding and landslips. water - level information from the northern part of the new territories is also similarly relayed to the observatory for real - time monitoring of floods in these areas
一個由超過70個分佈於香港境內的自動雨量器所組成的網路,將最新的雨量數據傳送到天文臺總部,即時提供評估水浸及山泥傾瀉可能性的重要資料。此外,新界北部河流的水位資料亦傳送至天文臺總部以實時監測該區的水浸情況。But on the later condition the trend of accumulation turned to be stable in the w3 treatment ( vseawater / v pure water = 1 ) - in root zone soil, variation of sar value accorded with total salt accumulations and sometimes decreased at the treatment where the v seawater / v pure water > 1. contents of cl - and na + which were the main ions and leached obviously in 0 - 60cm soil were greatly influenced by rainfall, but the rainfall did not affected the contents of ca2 +, mg2 + and k + whose ability of leaching is worse than that of cl - and na + in the root zone soil obviously. the vertical distribution of salt ions in the 0 - 60cm soil were mainly affected by the ratio of v seawater / v pure water in the irrigation water on the condition of not enough rainfall, but on the cont
海水灌溉下,耕層土壤中鹽分含量受降雨量影響很大,足夠的降雨條件下,鹽分不會積累,降雨量較低時,鹽分積累明顯,但在50海水處理下趨于平衡狀態;耕層土壤sar值的變化情況和鹽分含量變化情況相一致,在灌溉水中海水濃度大於50時有所下降;土壤中主要鹽離子為cl ~ -和na ~ + , 0 - 60cm土層內, na ~ + 、 cl ~ -明顯的向土壤底層遷移,其在土壤中的含量受降雨影響顯著,而ca ~ ( 2 + ) 、 mg ~ ( 2 + )和k ~ +在土壤中遷移能力較低,其含量受降雨影響較小; 0 - 60cm層次土壤鹽分的縱向分佈在降雨量較低的條件下主要受灌溉水中海水濃度的影響,而在降雨充分的條件下,地面覆蓋程度成為重要的影響鹽分和水分脅迫下菊芋的生理響應及其海水灌溉研究因子之一。This system calculates the movement of rain areas detected by weather radars and then projects from these movements the rainfall in the territory
該系統利用氣象雷達探測所得降雨分佈情況,計算降雨區的移動速度,從而推算香港境內的雨量。A map showing the rainfall distribution over the territory up to 1 p. m. today is attached in
顯示本港今天直至下午1時的雨量分佈情況。For the rainfall distribution in hong kong today, please refer to the rainfall distribution map below
有關本港今日雨量分佈情況(至下午7時) ,可參考以下雨量分布圖。5 - day weather forecast ). a rainfall distribution map for today ( wednesday, 11 june 2003 ) up to 6 p. m
本港今天( 2003年6月11日星期三)雨量分佈情況(至今日下午6時為止)Rain was heaviest around 10 a. m. to 11 a. m. figure 1 shows the rainfall distribution over hong kong today till 6 p. m.
有關本港今日雨量分佈情況至下午六時為止,可參考圖一。分享友人