cloud paper 中文意思是什麼

cloud paper 解釋
雲彩花紙
  • cloud : n 1 雲。2 雲狀塵埃、煙（等）；（鳥、蟲、飛機等的）大群，大隊。3 （水晶等的）霧斑，（鏡子等上的）...
  • paper : n 1 紙；裱墻紙。2 報紙，報。3 收據；債券；證券；票據；匯票；鈔票（＝paper money）。4 〈pl 〉身份...
  1. In this paper, four cases of heavy rainfalls and snowfalls in china are simulated by using mm5. cloud microphysical characteristics and sources of rain, snow and graupel have been particularly studied

    運用中尺度非靜力數值模式mm5v3 ，對我國華南前汛期暴雨、梅雨鋒暴雨、北京東風迴流降雪和遼寧寒潮大風雪等四次過程分別進行了模擬研究。
  2. 3d - image of cloud has a great advantage in weather forecast over 2d - image of cloud. in this background, this paper studies the 3d - visualization of cloud based on infrared nephogram of satellite. the main content is as follows : 1

    三維化衛星雲圖的優點是顯而易見的，同二維雲圖相比，比較明顯地顯示整個大氣空間雲團的分佈及結構，增強不同層次的對比度，因而更易分辨出大氣系統，可以為大氣預報提供直觀的依據。
  3. Avionics self - protection system is a subsystem of the advanced avionics system, which has the main functions to find hostile radar - guided weapons system and infrared - guided weapons system by using the mothed of radar reconnaissance. and then to countermeasure enemy ' s radar - guided weapon system and infrared - guided weapons system by adoptinging those measures of electric - magnetic jamming ( active countermeasures ), chaff cloud deception jamming ( passive countermeasures ) and ir decoy deception jamming ( passive countermeasures ) so as to protect our airplanes from the hostile attacks this paper have researched deeply for the integrated mode of avionics self - protection system

    航空自衛系統是先進航空電子綜合化系統的一個分系統，其主要功能是通過雷達偵察方式發現敵方雷達制導武器系統和紅外製導武器系統，並通過實施電磁干擾（有源干擾） 、箔條雲欺騙式干擾（無源干擾）和紅外誘餌欺騙式干擾（無源干擾）對抗敵方雷達制導武器系統、紅外製導武器系統，保護我機免受敵方武器系統攻擊。
  4. The fundamentals and method of deducing path - integrated cloud liquid water content ( l ) by an airborne up - looking microwave radiometer are introduced in this paper

    在這種情況下，本文對對空機載微波輻射計的反演方法進行探索。
  5. This paper presents two methods for cloud detection : multi - channel dynamical threshold algorithm and apparent reflectance algorithm

    本文介紹了兩種雲檢測演算法：雙通道動態閾值法和表觀反射率法。
  6. There is a vaporizing layer below 0 layer and it is far thick, which may be one of the important reasons of small precipitation on ground ; in the paper the cloud and the rain drop size distribution in warm layer of stratiform cloud are calculated and analyzed. it is found that n ( d ) = n0dnexp ( - a d ) can express the size distributions of little cloud drops, big cloud drops and rain drops. the observational and calculated results are well matched

    在零度層以下蒸發層的存在，且比較深厚，應是導致地面雨強較小的重要因素之一；本文對暖層的雲滴譜和雨滴譜進行了計算，對小雲滴、大雲滴和雨滴分佈可以用同一種形式的分佈密度函數多階函數n （ d ） = n _ 0d ~ nexp （ - d ）來表示。
  7. In the second part ( including chapter 4 ), this paper applies gray level coocurrence matrix and image texture feature quantities to evaluate eliminate effect through computing the same sampling region selected. the results show that the three methods can eliminate solar eclipse impact on the satellite vis imagery so that the topography, cloud system texture and ocean current are distinct and differentiable and it is good for analyzing the clouds and weather systems on the cloud image. comparing the three methods, the improved geometry - model method is the most effective

    研究結果表明：原幾何模型法、改進的幾何模型法和數學函數模型法基本都能消除日食對雲圖的影響，經過訂正處理后，各種特徵紋理變細，結構變清晰，信息增加，有利於雲圖上雲和天氣系統的識別和分析；三種方法的比較認為，改進的幾何模型法訂正效果最好，原幾何模型法的效果較差，數學函數模型法更加快速、簡便，但其涉及的主觀因素較多。
  8. He in childhood uses innocent and curious studying in a mountain village with charming scene of east pinggu in beijing in liu ruiyou ' s hometown, look at blue mountains and green waters, white cloud blue sky that, is it blow colorful dream to make at night, pairs of pictures depicted with plain and clumsy lines have appeared on the paper on the ground on the wall

    劉瑞友的家鄉在京東平谷一個風光旖旎的山村裡童年的他用天真而好奇的研究，望著那青山綠水、白雲藍天，夜裡便做起了五彩繽紛的夢，墻上地上紙上便出現了一副副用稚拙的線條描繪出的畫。
  9. In this paper aircraft has made vertical and synthetic detecting flying purposefully on 9. 17, 2003 according to cloud ' s macro and microstructure. vertical layers and representative places of stratiform cloud on 9. 17, 2003 are analyzed using the observational data of particle measurement system ( pms ), combined with satellite data, radar data, and precipitation data on ground. by this we have got cloud ' s microphysical structure and physical process of the natural precipitation, and the physical effect evidence has been testified according to observational data after lco2 seeding

    本文用綜合觀測的方法，利用機載pms雲粒子探測系統，根據雲系的宏微觀結構特徵進行有針對性的垂直探測飛行，配合衛星、雷達、地面雨量、雨強計網觀測資料對2003年9月17日延安降水性層狀雲系中那些有代表性的部位或垂直分層做細致的觀測分析，獲得雲系的微物理結構和自然降水形成的物理過程，並用觀測事實來驗證人工增雨引晶催化后的物理響應判據。
  10. In the paper using the cloud particle characteristics and particle spectrum data in different heights, the vertical macro and microstructure or the coagulation water phase can be partitioned into 5 growth layers

    本文通過對不同高度上的粒子特徵量和譜分析，降水性層狀雲宏微觀垂直結構配置或水凝物主要特性可以分為5個發展層。
  11. The paper uses the surface radiation observations from 08 to 17 o ' clock and the visible, infrared digital cloud picture from gms4 at the same time over beijing, tianjin, jinan, taiyuan, hefei, nanjing, shanghai area in june and july 1994

    本文利用1994年6月、 7月北京、天津、濟南、太原、鄭州、南京、合肥、上海地區地面凈輻射觀測資料及同期gms衛星紅外、可見光數字雲圖資料。
  12. In this paper, we take the reconstruction of surface of revolution as our main aim, and by using the delaunay triangulation, the definition of curvature and the theory of b - spline, we present a way of reconstructing surface of revolution from point cloud. the main content of this paper is given in the following. computer aided geometric design and reverse engineering are the basis of this article

    本文以旋轉面重建演算法為主要研究對象，應用三角部分、曲率的定義以及b樣條理論提出了一種由點雲數據構造旋轉面的方法，主要工作如下：計算機輔助幾何設計以及反向工程是本文的理論基礎，因此論文的第一章對其進行了簡短的回顧和綜述，並給出了旋轉面重建演算法目前的研究狀況。
  13. This paper is based on summarizing and analyzing the correlative work. it introduces the speed of the uniform flow closing to the dynamical field in the factual cloud to the answer of the probability equation of the catalyst particle remains in the cloud of nucleation layer, ameliorates the answer of the equation which does n ' t consider the uniform flow evidently

    本論文在總結分析已有相關工作的基礎上，對催化劑粒子在雲中核化層存留概率方程解中，引入了和實際雲中動力場相近的均流速度，明顯改進了過去不考慮均流的概率方程解。
  14. The paper works out the ice crystal spectrum distributing in the different macroscopic and micro - backgroud of the cloud ( ie, the thickness, the temperature and the supersaturation with respect to ice of the nucleation layer ). this paper also works out the amount of catalyst which is allowed in the cloud nucleation layer according to the different quantity of the supercooled water, the density of the supersaturation of the vapor with respect to ice. simultaneously, the paper discusses the i nfluence of remaining time when seeding artificial ice nucleus in the different ascending - velocity and altitude, and elicits the proper seeding altitude of the catalyst

    以此解為依據，得出了不同均流時，人工引入冰核在核化層存留時間，再以此時間作為人工冰核凝華增長時間，求出不同的雲宏微觀背景（如核化層厚度、溫度、冰面過飽和度等）下的冰晶譜分佈，經和實際資料比對符合相當好。進而求出核化層中不同過冷水量、冰面過飽和水汽密度下雲核化層可允許的催化用量。同時討論了不同升速，不同高度引入人工冰核時對其存留時間的影響。
  15. In this paper a system has been developed for studying characteristics of " clouds and sky " on the images taken by a whole - sky camera at three different wave bands ( the visible, the infrared, long wave infrared ), then assessing the presence, distribution, shape, and radiance of clouds over the entire sky using automated cloud decision algorithms and related processing

    根據發展自動化雲觀測的目標，利用雲和晴空大氣在可見光近紅外、熱紅外多波段散射輻射和熱輻射的不同特徵，我們嘗試建立一個多波段（可見近、熱紅外）全天空成像輻射觀測系統，進行全天空分波段成像輻射的獲取，定量分析和特徵識別，獲得雲量、雲型、雲底高信息，實現對雲參數化信息的自動獲取。
  16. Based on earlier research results, this paper aims at improving the forecast skill for rainfall by experiments, which add satellite infrared cloud image into a forecast model mm5 quantificationally

    為了提高數值預報模式的強降水預報能力，本文在前人研究成果的基礎上，主要從事應用性試驗研究。將現有的靜止氣象衛星紅外雲圖資料定量加入到模式中。
  17. In terms of cloud condition, the results are improved when data of irl minus ir3 are used, which give a new method to study cloud effect on net surface radiation. in this paper, an new index named crci, cloud radiation control index, is adopted. crc1 can describe the relationship among cloud reflecting radiation, cloud emitting, earth - atmosphere radiation and surface radiation balance

    為了充分表達雲對太陽輻射、地球大氣輻射的控製作用，本文還引入了雲輻射控制指數（ cloudradiationcontrolindex ， crci ） ， crci可以反映出不同的雲量、雲的光學特性等因素對雲反射太陽輻射、雲自身發射的紅外輻射、地球大氣輻射和地面輻射收支間的關系。
  18. This paper comprises two parts : radar clutter simulation and adaptive moving target indication. in the former part, we analyse the generation mechanism of single - channel radar correlated clutter and illuminate the simulated modeling way of rayleigh, log - norm, wei bull, k - distributed clutter with special power spetrum. all these models are used into the practical simulation of ground clutter, cloud - rain clutter and chaff jammer according to their features

    在雷達雜波模擬部分分析雜波的產生尤其是單通道相關雷達雜波產生的機理，具體闡明了在指定雜波功率譜情況下，幅度服從瑞利分佈、對數正態分佈、韋伯分佈和k -分佈的雜波的建模與模擬方法，並根據不同分佈的特點，將其應用到地雜波、氣象雜波和箔條干擾的模擬中。
  19. The paper discussed a method which automatically detect cloud in polar orbit meteorological satellite images by using visual band reflectance and thermal infrared bright temperature

    本文探討了利用極軌氣象衛星圖像可見光波段的反射率和熱紅外波段的亮溫信息進行雲自動檢測的方法。
  20. The cloud shortwave radiative forcing was studied by using gms satellite data and the routine data in the typical 9 stations in the paper

    本文利用gms衛星資料和常規資料研究雲對輻射的作用，對中國大陸地區比較有代表性的九個站點夏季每日08 、 09 、 10時的短波雲輻射強迫進行了研究。
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