氣候變換 的英文怎麼說
中文拼音 [qìhòubiànhuàn]
氣候變換
英文
klimawechsel atmospheric change-
The coal conversion technologies that come to dominate will be those that can meet the objectives of climate change mitigation at the least cost
未來，那些價格最低、又能延緩氣候變遷的煤轉換技術，將成為主流。By using ncep / ncar reanalysis data of height and wind, the inter - monthly lpac map, the climate lapc map, inter - annual anomaly map and mean variance map of monthly wind field of 850 and 500hpa and monthly height field of 850, 500, 150, 30hpa are calculated in a globe - belt area, which situates between 30 s and 75 n, from december 1957 to december 1997, according them we analysis the rule of the season transfer and anomaly of nh mean circulation. the results show that the climate map of lapc can describe the seasonal transfer process of large scale circulation better. the advance process of summer circulation establish is form south to north at the middle and lower level of the troposphere, that is reflected primly in the inter - monthly wind and pressure map of lapc ; at lower lever of stratosphere, the establish process is simulate to that of troposphere, and reflect of process of that the south asia high toward plateau ; at middle stratosphere the summer circulation establish begins at middle and high latitude initially, and then transmits to low latitude gradually, while the seasonal variability in mid - stratosphere is stronger than it in troposphere and low - stratosphere
利用ncep ncar再分析高度場和風場資料，計算了30 s 75 n球帶區域1957年12月至1997年12月逐月850 、 500hpa風場及850 、 500 、 150 、 30hpa高度場月際局地型相似系數圖、多年平均圖（即氣候lpac圖） 、年際異常圖及均方差圖，在此基礎上，分析了北半球平均環流季節轉換及其異常的規律。分析表明，氣候局地型相似系數圖較好地給出了大尺度環流季節轉換發生的過程：在對流層中、下部，風、壓場月際局地型相似系數圖清楚地反映了夏季型環流建立由南向北的推進過程；低平流層夏季型環流的建立與對流層接近，其中，南亞高壓上高原過程有明顯反映：中平流層，夏季型環流的建立明顯表現為從中、高緯度開始，逐步向低緯傳播的特徵，且變化較對流層和低平流層明顯。The results were shown as follows : ( 1 ) based on weather data, the space - time changes of climate in chongqing karst region were analyzed applying regression analysis and kriging interpolation and the future climate was forecasted by wavelet analysis
主要研究結果如下： （ 1 ）利用回歸分析、 kriging空間插值等方法分析了基於氣象數據的氣候的時空變化，並採用小波變換對未來的氣候進行了預測。In other words an unstable climate will make the very kinds of tensions and conflicts that the security council deals with, day in day out, yet more frequent and even more severe
換句話說，隨著時間的推移，不穩定的氣候因素會使聯合國安理會處理的各種緊張局勢和沖突變得更加頻繁和嚴峻。Adaptation to climate change in date of seasonal dressing change in beijing during late 19th century
19世紀後半葉北京地區人的季節性換裝對氣候變化的適應The clm was originally developed by dr. dai yongjiu on the basis of the bats 26, ncar lsm 27, and iap94 28, which have been already adopted by the ncar ccsm 29. the clm mainly represents inter - actions between the atmosphere, vegetation and land, and reflects the change of the water, heat state and the transfers of heat and water. soil moisture in this model is predicted from a ten - layer model fixed depth
Clm是由戴永久博士在bats 27模式ncar lsm 28 ， iap94 29的基礎之上開發出並為美國國家大氣研究中心的氣候系統模式ncar ccsm所採用的陸面模型30 . clm模式主要考慮慮了大氣植被土壤之間的物質交換過程，反映土壤植被大氣中水熱狀態變化和水熱傳輸( 3 ) though the conventional fourier power spectral analysis can reflect the common characteristics of the signal, it cannot provide the fine structure of time - frequency changes and the location of the jump points, while the wavelet transforming can better the situation
傳統的功率譜分析方法雖然能反映氣候信號變化的一般特徵，但無法反映時頻域變化的精細結構，也不能給出突變點的具體位置；而小波變換分析方法則可以很清楚地給出氣候信號變化的多層次結構和突變特徵。Methane and nitrous oxideare taken into account by converting them into “ carbon - dioxide equivalent ” emissions using conversion factors provided by the intergovernmental panel onclimate change
人們已經在考慮將沼氣與一氧化二氮氣體使用由氣候變化政府專門小組提供的轉換因子轉換為二氧化碳的對等物。分享友人