climate anomaly 中文意思是什麼
climate anomaly
解釋
氣候異常-
In addition, the ao index released by american climate prediction center ( cpc aoi ) fails to reflect the summer ao mode. in this paper, the time series of the leading principal component of the summertime ( june - september ) surface level pressure anomaly field over the domain poleward of 20 n is defined as the summertime ao index
此外，美國氣候預測中心發布的全年北極濤動月指數不能表現夏季北極濤動型，本文將北半球熱帶外地區（ 20 n以北）夏季（ 6 - 9月）海平面氣壓場eof主模態的時間序列定義為夏季北極濤動指數。 -
The relationship between sea surface temperature anomaly in pacific and the circulation of northern hemisphere is the focus of air - sea interaction research in recent years. the ssta in pacific contributes to remote response in mid - latitude atmosphere, and is connected with climate changes in global. the cycling of enso is typical phenomena of large scale in pacific air - sea interaction system
太平洋海溫異常對北半球大氣環流異常有重要影響，而enso循環是太平洋海氣耦合系統中典型的異常演變過程，不僅描述了熱帶地區大氣和海洋異常現象，而且與中高緯度的氣候異常變化相聯系。 -
Effects of climate anomaly on grasshopper in the pasture areas around around qinghai lake
氣候異常對青海湖環湖地區草地蝗蟲災害發生的影響 -
In order to study the anomaly pattern of summer rainfall in north china and the cause responsible for the anomaly, the climate characteristics of summer rainfall in north china and related circulation pattern, water vapor transport and outgoing long - wave radiation ( olr ) were analyzed in detail in this paper. more attention was paid on studying the relationship between sea surface temperature anomaly ( ssta ) over the north pacific and summer precipitation anomaly in north china and an agcm was utilized to confirm the affection of ssta on the summer rainfall of the north china
為了揭示華北夏季降水異常規律及其成因，本文詳細分析了華北夏季降水的氣候特徵及有關的環流特徵、水汽輸送特徵和向外長波輻射（ olr ）特徵，著重研究了北太平洋海溫異常與華北夏季降水異常的關系，並應用大氣環流模式初步驗證了北太平洋海溫異常對華北夏季降水的影響。 -
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。 -
In terms of the real data, the mass stream function is calculated by two methods, results indicate that both methods fit well with the need for calculating the climate and its anomaly of the mean meridional circulation
本文通過實際資料的計算比較了質量流函數的兩種計算方案，驗證了簡化方法同樣適用於平均經圈環流的氣候及其異常的分析需要。 -
Using monthly mean rainfall and temperature data in north - west of china ( nwc ), the characteristics of rainfall anomaly at rainy season in nwc and the inter - annual varieties of drought / flood are diagnosed by means of eof, reof and wavelet analysis et al. and the ncep / ncar monthly reanalyzed data are employed to analyse the evolution character of water vapor flux and it ' s divergence flux, 500hpa height and u, v wind field. results show that ( a ) the space distribution of rainfall anomaly can be separated into seven climate sensitive areas, the first and the third region have the same rought / flood trend
本文使用西北（區） 168個站1961 2000年6 9月（主汛期）月平均降水、溫度資料，運用eof 、 reof 、小波分析等方法診斷了主汛期月降水異常和旱澇的年代際變化；同時利用ncep ncar月平均資料，分析了強（弱）季風年西北空中水汽通量及其散度場、 500hpa高度場、 u 、 v風場的演變特徵，結果表明： （ a ）西北汛期降水可分為七個氣候異常區，第一、三異常區旱澇趨勢相同。 -
A standard practice to minimize the impact of the model systematic error is to calculate the anomaly from " model climate " rather than from the observed climate
計算模式氣候是相當費時的工作。現時天文臺是以1998至2001年間rcm的輸出來運算模式氣候，並假設模式氣候是接近常態分佈。 -
3 ) the anomaly interaction of global sea thermal elements with climate elements is of persistence from previous summer / winter through current winter / summer with relative stable interaction areas on inter - decadal time scale. while their abrupt climate change did not occur simultaneously
3 ）在年代際尺度變化方面，海洋熱異常和氣候異常有較好的同期相關關系，相互作用的關鍵區也有較穩定的位置，不同要素的氣候躍變點不盡相同。 -
Results show that the climate and anomaly field of monthly mean temperature is characterized by low - order
分析揭示了月平均溫度氣候及其異常場集具有低階、低維的特徵。 -
The results are outlined as following, 1 ) anomaly fields have their larger inter - decadal component percentage but smaller inter - annual one in both climate and sea thermal elements
結果表明： 1 ）年代際變化在海洋要素和氣候要素異常的構成中均是顯著的，而這些要素對應的年際變化冬夏均不顯著。 -
5 ) the spatial distribution pattern of sea surface temperature anomaly over the east pacific is related to el nino, as indicates inter - decadal climate oscillation for the strong inter - annual events
5 ）海洋熱異常尤其是東太平洋的空間分佈反映出類enso模態的特徵，體現了年際信號同時具有年代際尺度的變化。 -
Relationship of east siberian autumn sea ice anomaly with winter atmospheric cir culation and east asia climate
秋季區域海冰面積異常與冬季大氣環流及東亞區域氣候的關系 -
By using multi - channel observations of olr, hirs - tb12, erb, vis, ssmr and ssm i on the us satellites, it is analyzed that the global general atmospheric circulation features related to the anomaly of cold vortex over northeast china and it s premonitors are also revealed. it is found that there is an effected chain, which consists of sea ice over northern hemisphere, sea surface temperature in the mid - east equatorial pacific, asia monsoon and local budget of earth radiation in northeast china, on the anomaly of northeast cold vortex. the impacts of each factor in the chain are discussed. the results indicate that the applications of multi - channel satellite observations on research of climate change are of significance
利用美國氣象衛星olr ， hirs - tb12 ， erb ， vis ， ssmr和ssm i多通道的觀測資料，分析了東北冷渦異常年的全球大氣環流特徵及其關鍵地區的先兆特徵對于東北冷渦異常，發現了有一個由北半球的海冰，赤道東太平洋的海溫，亞洲的季風以及東北地區地氣系統輻射收支組成的影響鏈存在。由此討論了影響鏈上的各因子對東北冷渦異常的作用。結果表明多通道衛星觀測資料的綜合應用在氣候變化的研究和預測中有著重要的意義。 -
In addition, this paper primarily analysis the anomaly characteristic of 1980 and 1991 using the climate and anomaly map of lapc
此外，論文還用氣候lpac圖和異常lpac圖對1980和1991年異常的特徵作了初步分析。 -
In order to study the anomaly pattern of summer rainfall in north china and the cause responsible for the anomaly, the climate characteristics of summer rainfall in north china and related circulation pattern of lower, middle and upper layer of prophase and the same time were analyzed in detail in this paper
為研究華北夏季降水的異常規律及其成因，本文詳細分析了華北夏季降水的氣候特徵，以及前期和同期的低、中、高層的環流特徵。同時還分析了華北夏季降水異常的物理量場的特徵。
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