change from season to season 中文意思是什麼
change from season to season
解釋
隨季節變化-
It also explain that the correlation between ssta of kuroshio and the change of wind field in equaroral mid - pacific is results of air - sea interaction ; however, when time comes into summer, the instance status of ocean is different from the last winter to next early springtime, the sea surface temperature turn into the definitive factor, so the increase of heat flux in may to jun month which is realized by absorbing more heat from the sun radiation results in the decrease of sst in kuroshio in the season of jun - jul. finally, during the aug to dec season of next year, the sst of kuroshio is increasing again
最後分析了黑潮海溫與夏季東亞大氣環流及我國降水的時滯關系，發現：當前冬黑潮區域海溫異常偏高時，後期夏季亞洲低壓的強度減弱，西北太平洋副熱帶高壓強度加強，而且位置西伸、偏北，梅雨鋒位置偏南，長江中下游地區降水偏多，北太平洋冬季海域的海溫分佈呈+ 、 - 、 +趨勢（順序為赤道中東太平洋、西北太平洋、我國近海） ；反之亦然。 -
In a year the change of river flow is drastically and season distributes of runoff in river is mainly centralize in the summer in jia - lu - he, qiu - shui - he and pian - guan - he catchments. for example, the runoff amount from july to august accounts for 41 %, 58 % and 57 % of the annual runoff amount in the above three catchments, respectively
所選四條流域中，佳蘆河、湫水河和偏關河三條河流徑流量年內變化劇烈，季節分配不均，集中度高， 7 8月份徑流量分別占各流域年徑流量的41 、 58和57 。 -
Results show that the interdecadal anomalies are more significant in the variance of the system anomaly in the north pacific ( np ), and the interannual and interdecadal anomalies are about equivaleut in the tropical pacific ( tp ) ; the interdecadal change characters of the surface ( shallow ) layer of the ocean and the atmosphere aloft are unanimous in the same season and region, and their transition from a low mode to a high mode both occurred from the end of 1970s to the beginning of 1980s, with an exception for july in the np, which is related to the stability of the stratification of sea temperature within the sub - surface layer ; the interannual scale air - sea anomalies are associated with enso, is most typical for january, then july in the tp, followed by january in the np, and there is no visible relationship for july in the np
在海氣系統異常的方差構成中，北太平洋區域以年代際異常為主，熱帶太平洋區域年際和年代際異常相當；表（淺）層海洋與大氣的年代際變化特徵對同一季節、區域是一致的，且20世紀70年代後期到80年代初均發生由低模態向高模態的轉變；北太平洋區域的7月與此不同，這與該季節近表層海溫層結穩定有關；年際尺度的海、氣異常與enso有關，且以熱帶太平洋區域1月最典型， 7月次之，北太平洋區域1月再次之， 7月無明顯關系。 -
In this study, we demonstrate a technique using the multi - temporal c band hh polarized radarsat scansar data to estimate the relative soil moisture change. the experiment data from sgp97 covered a whole range of vegetation growing season and different type agriculture fields
研究證明，星載合成孔徑雷達（ sar ）得到的地表後向散射系數與地表介電常數有直接相關關系，從而能夠在水文模型要求的精度范圍內有效提取地表土壤水分信息。 -
It can be found that a great quantity of vapor is transported to atmosphere from arctic ocean open sea in summer, which is very important to concerns on season change of heat budget on arctic ocean
由此可見，在北冰洋夏季，無冰海面有大量的水汽向大氣輸送，這對研究北冰洋地區大氣邊界層的季節變化過程是至關重要的。 -
The changing trend of the range with season is not apparent, but the ranges change from 3. 02m to 39. 29m
變程的變化幅度大，在3 . 02m和39 . 29m之間波動，但季節變化趨勢並不明顯。 -
Using monthly and daily mean temperature data from 726 stations ' s across china mainland for period of 1951 to 2001, the author established the time series of mean temperature for the region, and analyzed the decadal variation and change trend in temperature and temperature - defined growing season over the past 51 years
利用中國726個站點1951 - 2001年的逐月和逐日平均氣溫記錄，分析研究了中國1951 - 2001年氣溫和1961 - 2000年溫度生長期的變化及其趨勢。結果表明， 1951 - 2001年期間，中國氣溫上升明顯，增暖過程從80年代開始， 1987年以後，增暖趨勢有了進一步加快的趨勢。
分享友人