Through simulating the speckle intensity distribution in the far field of a random rough surface,we compute the degree of angular speckle correlation by substituting spatial average in speckle pattern for conventional ensemble average,and determinate the surface roughn.

通過模擬計(jì)算隨機(jī)粗糙表面的遠(yuǎn)場散斑場富婆按摩高潮对白在线观看，以散斑圖面上的空間平均代替常規(guī)的集平均來計(jì)算角度散斑相關(guān)系數(shù)欧美性爱老牛视频，并應(yīng)用集平均的數(shù)學(xué)模型反演粗糙度參量人人操人人草人人爱。

Through simulating the speckle intensity distribution in the far field of a random rough surface, we compute the degree of angular speckle correlation by substituting spatial average in speckle pattern for conventional ensemble average, and determinate the surface roughness by the mathematic model of ensemble average.

通過模擬計(jì)算隨機(jī)粗糙表面的遠(yuǎn)場散斑場，以散斑圖面上的空間平均代替常規(guī)的集平均來計(jì)算角度散斑相關(guān)系數(shù)午夜激爽免费毛片，并應(yīng)用集平均的數(shù)學(xué)模型反演粗糙度參量久久亚洲这里都是精品。

The concept of the weighted logarithmic power mean is introduced; its relation with two-parameter mean is given; the inequality for weighted logarithmic power mean is derived; the magnitude relation among upper bounds of geometric mean and arithmetic mean of geometrically convex functions are made certain.

建立了幾何凸函數(shù)的對稱擬算術(shù)平均不等式，對文獻(xiàn)[1]提出的不等式進(jìn)行了推廣統(tǒng)一国产黄片毛片视频；引進(jìn)加權(quán)對數(shù)冪平均的概念女人插插插视频，建立起其與雙參數(shù)平均之間的關(guān)系，得到加權(quán)對數(shù)平均不等式一级毛片性爱视频网站，從而確定了幾何凸函數(shù)的幾何平均欧美性爱欧美性爱欧美性爱、算術(shù)平均的上界的大小關(guān)系；最后中文字幕丝袜无码第一页，提出了幾何凸函數(shù)的對稱擬算術(shù)平均不等式的推廣問題天天做天天干天天日天天舔。

Uses the arithmetic mean of the mean peak force and the mean valley force.

4使用算術(shù)平均的平均峰值力及平均谷武力。

With the meridional method and based on observational data, the features of uniform subtropical high belt are diagnosed. Results show that for the annual and zonal mean subtropical high, the interannual variability is very small and could be neglected.

依據(jù)經(jīng)向偏差的分解方法日本人黄色免费网站，對均勻副高帶氣候平均的特征進(jìn)行了資料分析研究曰本一级AAAA片无码，發(fā)現(xiàn)年平均的緯向平均副高帶的年際變化很小国产精品久久五月丁香，可以忽略。

Based on the review of the description of subtropical high and the research on its formation, fluctuation characteristics and physical mechanisms, it is found that the subtropical high is refered to the area where pressure is relatively larger. Its formation is due to the existence of mean meridional circulation that accumulates air mass to subtropical areas. The subtropical high is belt-like with meridionally non-uniform feature and this is a zonal mean point of view.

通過對副高的描述精品九久、形成及演變特征和物理機(jī)理的研究進(jìn)行回顧激情文学,图片区,视频区,偷拍，認(rèn)為：副高是相對的氣壓的高值亚洲精品笫一页国产精品，是由于平均經(jīng)圈環(huán)流的存在91亚洲高清无码视频，使得有空氣質(zhì)量在副熱帶地區(qū)的堆積而形成的，成為帶狀欧美自拍日韩免费观看，表現(xiàn)出在經(jīng)度方向的不均勻精品不卡一区中文字幕，這是一種緯向平均的觀點(diǎn)；同時(shí)欧美牲爱视频，在這個(gè)平均的高壓帶上常常有閉合的單體存在无码中文字幕一级毛片，表現(xiàn)出緯向的不均勻。

According to the energy conservation theory, BOM and CSIM4 were coupled. The BOM has no treatment on transmission solar radiation, which is of great importance when the model is adapted to Arctic Ocean. So the treatment was introduced to BOM. Through numerical test on different lead albedos, it was found that sea ice thickness is not so sensitive to lead albedo, which may be contribute to the lead occupies little ratio within multiyear sea ice pack. The reason of summer over-melt of arctic sea ice is the NCEP reanalysis downward solar radiation being larger than its reality. Then the arctic sea ice climate variability was simulated. Results showed that: simulated ice thickness change is in accord with the submarine investigated mean sea-ice draft changes. Simulated annually maximum ice thickness along the Eurasian continental oceans are closely related to the observed ones. The long-term mean simulated ice motion has the same features of the SSM/I derived ice motion. Sea ice extents in differential sub-regions have same trends comparing to the satellite passive-microwave data derived ones. Simulated ice concentration is closely related to the observed in the Arctic sub-regions. Sea ice flux through the Fram Strait involves ice concentration, motion and thickness. It is a composite criterion for sea ice model evaluation. The simulated ice area and volume export through the strait accord with the satellite derived or statistically reconstructed ones.(5) The simulated ice thickness climate variability and mean sea surface current of the coupled model were analyzed, results showed: the total ice volume in the Arctic Ocean has a significant decreasing trend. The volume variability is of a 10-year timescale oscillation, with two major periods of 12-13a and 18-20a. Mean ice thickness in the arctic sub-seas has different tendencies. It has an increasing trend in the Barents-Kara Sea and Baffin Bay-Labrador Sea, and decreasing in the others. The characteristic time scale of 7-10a wherein the river discharges leads the Fram Strait ice volume export is about the period that river water takes to be conveyed across the Arctic Ocean.(6) Using the simulated ice distribution in the Arctic Ocean and China precipitation, air temperature and SST in tropical key regions, the climate teleconnection were studied. Result showed: When the mean sea ice thickness is large in the central Arctic Ocean and Chukchi-Beaufort Sea , and small in the Barents-Kara Sea and Baffin Bay-Labrador Sea , the precipitation in South China, Tibetan Plateau, and the north part of Northeastern China are always smaller than normal, and v. v. When the mean ice thickness is small in CA, BC, East Siberian Sea and Greenland-Iceland-Norwegian Sea , and large in BL, The air temperature in north-eastern China, the southern of Tibetan Plateau, and Hainan Island, are always lower than normal, and v. v. In addition, when the sea ice is thick in BC and BL, the SST is larger in the middle and eastern Pacific Ocean, and is smaller in the tropical Southeastern Indian Ocean.

由于BOM沒有考慮透射太陽輻射的物理過程欧美性v，研究表明透射太陽輻射對北冰洋的能量收支起到重要作用欧美性生活黄色网站，因此在BOM模式中引入了對透射太陽輻射的處理；通過對不同水道反照率的數(shù)值試驗(yàn)表明海冰厚度對水道反照率的敏感性不強(qiáng)欧美WWWWWWWWWW，可能與海冰區(qū)水道面積占的比率很小有關(guān)在线看黄片日韩黄；而模式模擬的北極海冰夏季&過度融化&主要源于NCEP再分析資料提供了偏大的太陽短波輻射；對北極海冰的氣候變率進(jìn)行了模擬研究性欧美69式XXXX，結(jié)果表明：模擬的海冰厚度變化與潛艇探測的海冰吃深度變化具有一致性一级毛片视频免费高清；模擬和觀測的亞歐大陸沿海的年內(nèi)最大海冰厚度有很好的相關(guān)；模擬的海冰移速與長期平均的衛(wèi)星反演的海冰移速具有相同的速度分布特征comwww啊好大轻点；模擬的各個(gè)海區(qū)海冰面積的變化趨勢與衛(wèi)星反演資料分析的結(jié)果基本一致特黄又大又粗又硬作爱大片；模擬與觀測的主要海洋分區(qū)的海冰密集度具有很好的相關(guān)：弗瑞姆海峽的海冰體積和面積的輸送涉及到海冰密集度、厚度和移動(dòng)速度欧美精品亚洲精品日韩传电影，是判斷模式模擬能力的一個(gè)綜合的指標(biāo)老女人性生活视频，模式模擬的結(jié)果與衛(wèi)星反演或重建的面積輸送、體積輸送具有很好的一致性亚洲色图欧美色图另类图片；(5)分析了模擬的北極海冰厚度的氣候變率及氣候平均表層海流場黄片免费动漫，結(jié)果表明：北極海冰的總體積有顯著減少的趨勢，北極海冰總體積的變化具有10a際尺度振蕩的特點(diǎn)国产天天干视频自拍，存在18-20a和12-13a兩個(gè)主周期无码又爽又刺激免费视频；北極海冰的平均厚度在各個(gè)海區(qū)的變化趨勢不同，在巴倫支—喀拉海和巴芬灣—拉布拉多海地區(qū)海冰厚度有顯著的增加趨勢久久久久久久妓女精品影院，而其它海區(qū)存在減少的趨勢久久精品国产精品久久人；通過對模擬的氣候平均表層海流的分析表明，北極河流流量超前弗瑞姆海峽海冰流量7-10年的特征時(shí)間尺度與表層海流的氣候分布存在著必然聯(lián)系：(6)利用模擬結(jié)果以及中國降水国产三级精品视频、氣溫和熱帶關(guān)鍵區(qū)SST資料永久黄网站色视频免费费，討論了北極各海區(qū)海冰平均厚度與中國降水、氣溫以及熱帶關(guān)鍵區(qū)SST的關(guān)系，結(jié)果表明：在北極中心海區(qū)和楚科奇—波弗特海海冰厚度偏大91伊人久久大香线蕉，在巴倫支—喀拉海以及巴芬灣—拉布拉多海海冰厚度偏小午夜无码一级成年大片在线69式，則中國降水在華南地區(qū)、青藏高原和東北北部降水偏少超碰个人免费，反之相反艹插舒服爽轮流视频；在北極中心海區(qū)、東西伯利亞海美女黄视频黄视频、楚科奇—波弗特海以及格陵蘭海海冰厚度偏小久久无码中文A片，在巴芬灣—拉布拉多海海冰厚度偏大，則在中國東北地區(qū)欧美一级特黄大片色视频、高原南部地區(qū)和海南島附近氣溫偏低日韩天堂2017，反之相反；另外级特大黄片视频影院8e，北極楚科奇—波弗特海和巴芬灣—拉布拉多海海冰厚度偏大時(shí)aaa黄色在线视频，在熱帶中東太平洋海溫偏高，而在熱帶東南印度洋海溫偏低欧美性爱b啪啪。

Also the seasonal variation of mean gedstrophic westerly, and the distribution of extra-long wave at this layer were analyzed.

分析了南半球?qū)α鲗?00hPa平均地轉(zhuǎn)西風(fēng)隨緯度的分布特點(diǎn)日本人伦影片，平均地轉(zhuǎn)西風(fēng)季節(jié)變化特點(diǎn)，計(jì)算分析了南半球位勢高度對緯向平均的偏差玖色综合，分析了超長波的分布特征国产超黄色视频。

In other words, regional mean runoff may be considered as the difference values between mean rainfall and infiltrations over a given heterogeneous land surface region, and the mean infiltration for the region may be calculated from two parts of infiltrations for saturation and non-saturation areas.

換言之，區(qū)域內(nèi)地表產(chǎn)流率可視為區(qū)域平均降水量與區(qū)域平均的土壤下滲量之差值潮吹国产，而區(qū)域內(nèi)土壤的平均下滲量又可分為非飽和區(qū)和飽和區(qū)兩部分的下滲量來分別計(jì)算小黄片真人视频毛片。

You will realize that the pebbles are generally closer to the mean distance then any other, because that's the definition of the mean.

我告訴你，因?yàn)槟愫軕信姑朗悠刀园粫?huì)自己動(dòng)手国产欧美亚洲精品a第二页，你有點(diǎn)懶散，你會(huì)發(fā)覺這些石子比任何其他的都接近平均距離午夜大香焦，因?yàn)檫@就是平均的含義9876se.色。

averagely：平均的

使---result in | 平均的:averagely | 估計(jì)是13%:estimated to be 13 percent

below average：低于平均水平的,差的

average 平均的,一般的 | below average 低于平均水平的,差的, | advanced 先進(jìn)的,高級的

below average：低于平均水平的,差的,來源:考試大

average 平均的,一般的 | below average 低于平均水平的,差的,來源:考試大 | advanced 先進(jìn)的,高級的

mass memory：中間的国产中文、平均的

Mark 機(jī)械国产一级黄色视频一区二区三区在线观看、力學(xué)、方法 | Mass memory 中間的人人伦av社区、平均的 | Master 間接的久久99精品久久久久久久清纯、調(diào)解

medial：中間的,平均的

mecometer 嬰兒身長測量計(jì) | medial 中間的,平均的 | median line 正中線,中線

resistant to：有耐藥性的 average 平均的

tolerate 耐受 | resistant to ......有耐藥性的 average 平均的 | minimum 最低(小)的

Of sample mean：樣本平均的

Of OLS estimators ...的OLS估計(jì)值 | Of sample mean 樣本平均的... | Sampling error 抽樣誤差

SMA：移動(dòng)平均

移動(dòng)平均分為簡單移動(dòng)平均(SMA)和指數(shù)移動(dòng)平均線(EMA). 指數(shù)移動(dòng)平均(EMA)與簡單移動(dòng)平均的數(shù)式十分相似. 技術(shù)分析員認(rèn)為較近期的數(shù)據(jù)更有參考價(jià)值,于是把較近期的收市價(jià)乘以更大比重,再除以比重的和,得出一個(gè)新的平均值.

averaged velocity：平均速度

average 平均值海損平均的按海損估價(jià)的 | averaged velocity 平均速度 | averagelifetime 平均壽命

Av. average：平均的;海損

AV Avenue 街道 | AV Average 平均的;海損 | AVR Automatic voltage regulator 自動(dòng)電壓調(diào)節(jié)器