陸半球 的英文怎麼說
中文拼音 [liùbànqiú]
陸半球
英文
[地理學] the continental hemisphere; the land hemisphere-
Satisfaction at the ubiquity in eastern and western terrestrial hemispheres, in all habitable lands and islands explored or unexplored the land of the midnight sun, the islands of the blessed, the isles of greece, the land of promise of adipose posterior female hemispheres, redolent of milk and honey and of excretory sanguine and seminal warmth, reminiscent of secular families of curves of amplitude, insusceptible of moods of impression or of contrarieties of expression, expressive of mute immutable mature animality
地球的東西兩半球所有已勘探或未勘探過的那些適于居住的陸地及島嶼午夜的太陽之國401幸福島402希臘的各個島嶼403被應許的土地404上,到處都是脂肪質女性臀部後半球散發出奶與蜜以及分泌性血液與精液的溫暖香氣,令人聯想到古老血統的豐滿曲線,既不喜怒無常,也不故意鬧別扭,顯示出沉默而永遠不變的成熟的動物性。Helicopters in action " is about to take you on an adventure around the world from sierra leone, where you ll participate in delivering humanitarian aid in the largest helicopter in the world, to miami for a wild ride in a black hawk helicopter intercepting drug runners. hold on while you swing through the air with five marines dangling from a rope attached to a ch - 46 flying over the atlantic and swoon as a cobra swoops low over enemy territory. try not to slip as you traverse 500, 000 - volt high wires
全天域電影直升機行動組將會帶你參與周遊列國的歷險旅程:在非洲獅子山你會乘坐全球最大型的直升機協助人道救援工作在美國邁阿密,你會登上黑鷹直升機截擊毒販又或者與五名美國海軍陸戰隊隊員一起乘坐ch - 46直升機,飛越大西洋上空,並在半空游繩而下或乘坐眼鏡蛇直升機在敵方領空低飛或登上直升機,跳上500 , 000伏特高壓電纜上進行維修工程或屏息靜氣,緊隨獸醫在南非乘坐直升機在離地面3米的高度,向黑犀牛發射麻醉槍或乘坐直升機跳入驚濤駭浪中參與海難救援工作。The interdecadal characteristics of correlation pattern of interannual relationship between winter sea - ice extent of davis strait and august 500hpa height of northern hemisphere is " + - + " pattern from ural mountains to north of sea of okhotsk which is strongly negatively correlated with the august rainfall of north china before 1974, and it has not apparent correlation pattern in europe - asia continent after 1974
1974年前,冬季戴維斯海峽海冰面積和北半球8月500hpa位勢高度場的相關系數呈一個自烏拉爾山開始到鄂霍次克海以北分佈的「 + - + 」型,該型和8月華北降水的反相關較好; 1974年後,相關在歐亞大陸地區變差,沒有明顯的相關型,冬季戴維斯海峽海冰面積和8月華北降水關系變差。In the northern hemisphere, the western portions of continents are especially favored by the prevailing winds.
在北半球,大陸西部地區尤受多風之惠。Thus, it can be clearly recognized that the global continents located at near equator and southern hemisphere, showed the characteristics of range along latitude ; chinese continental blocks still located among the laurentia, siberia and gondwana in paleozoic ; following the fast moving of siberia plate to northwards, the amalgamation in north - south direction at the western parts of laurentia and gondwana, subducted the lapetus and rheic oceans, until to form the uniform pangea in the late stage of paleozoic ; however australia and india plates in eastern gondwana move and disperse gradually to southwards, to extend crust and form the paleo - tethys ocean ; the chinese continental blocks and adjacent blocks still located in paleo - tethys ocean, preserved the status of dispersion, gradually moving to northwards, showed the characteristics of range along north - south orientation, until carboniferous and triassic a series of local collisions happened in tianshan - hing ' anling, kunlun, qinling - dabie, jingshajiang and shaoxing - shiwandashan zones, thus the most part of chinese continental blocks amalgamated to eurasia continent
由此可以清晰地看出,在古生代早期全球各大陸的主要部分都位於赤道附近及南半球,大致表現為沿緯度、呈東西向排列的特徵,中國及鄰區的小陸塊群在古生代始終都處在勞倫大陸、西伯利亞與岡瓦納大陸之間;隨著西伯利亞大陸的快速北移,在勞倫大陸與岡瓦納大陸的西部地區發生南北向拼合,亞皮特斯洋和里克洋的消亡,到古生代晚期形成統一的泛大陸;而岡瓦納大陸的東部(澳大利亞和印度等)則逐漸向南移動、離散,地殼張開,構成古特提斯洋;中國及鄰區的小陸塊群則一直處在古特提斯洋中,保持離散狀態,總體上緩慢地向北運移,並逐漸轉為近南北向的排列方式,石炭紀到三疊紀才在天山興安嶺、昆侖山、秦嶺大別、金沙江和紹興十萬大山等地段發生一系列局部性的陸陸碰撞,使中國大陸地塊的大部分逐漸併入歐亞大陸。( 2 ) ln winter of the northern hemisphere, because of the difference in the land - ocean distribution, the temperature nowadays is lower than that of 14mab. p. simulated in the upper layer but higher in the middle layer ( about 200 - 1500m ). in deep ocean the discrepancy of temperature seems hardly to be obvious
( 2 )北半球冬季,由於海陸分佈的差異使得海溫在海洋上層古海溫要暖于現代,在海洋中上層(約200 ? 1500米)現代的海溫則要暖於14mabBased on global land monthly precipitation dataset prec / l during the period of 1948 - 2001, ncep / ncar reanalyzed monthly mean wind data and global monthly sst grid data edited by british meteorological bureau. the flood / drought and the secular trend variation of precipitation of global, the northern hemisphere ( nh ), the southern hemisphere ( sh ), eurasia, africa, australia, north america, south america and antarctica in december - february ( djf ) are investigated
本文利用1948 - 2001全球陸地月降水資料( prec l ) ,美國ncep ncar再分析月平均風場資料和高度場資料以及英國氣象局整編的全球逐月海溫格點資料。研究了全球、北、南半球及歐亞、非洲、澳洲、北美、南美和南極大陸6個大尺度區域12 - 2月的降水趨勢變化及旱澇氣候變化。When the spatial pattern is of the north - south asymmetry, in the warm north - cold south years, there is a anticyclone circulation existing over the warm pool at 850hpa, easterly at 15 n and westerly in the tropical region have been greatly strengthened, while the center of anticyclone circulation moves to the east asia at 200hpa, and the hadley circulation has been affected evidently, so the summer rainfall may be above normal in the middle and lower reaches of the yangtze river, vice versa. there are different relations to east asia atmospheric circulation and summer rainfall in china
當ssta為南北半球反對稱分佈時,與ssta北暖南冷分佈相對應, 850hpa暖池區上空為一反氣旋偏差環流, 15 n附近東風氣流和赤道附近西風氣流增強,長江中下游地區盛行偏南風氣流; 200hpa反氣旋偏差環流中心移到東亞大陸上空;副熱帶高壓強度、西伸脊點都明顯變強、西伸; hadley環流得到發展,長江中下游(華北)地區為上升(下沉)氣流,降水明顯增多(減少) ,北冷南暖年則相反。The results indicate that the precipitation of global, nh and sh experienced decadal change : a minus - trend from 1974s global precipitation for djf, regression coefficient is - 0. 017mm / a
結果表明:全球、南、北半球的12 - 2月的陸面降水有明顯的年代際變化,全球12 - 2月降水量從1975年開始的明顯的下降趨勢,回歸系數約為- 0 . 017mm a 。When this precessional wobble brings the northern continents nearest the sun during the summertime, the atmosphere gets a notable boost of methane from its primary natural source ? the decomposition of plant matter in wetlands
當歲差的晃動讓北半球陸地在夏季與太陽距離最近時,大氣中的甲烷會明顯上升;而自然界中甲烷的主要來自於濕地植物的分解作用。The small landmass depicted on the southernmost part of the map is considered to be an imaginary continent, which was assumed to counterbalance the continents of the northern hemisphere, since the time of ancient greeks ( terra australis )
從古希臘時期起,小陸地被描繪在地圖的最南端,被認為是一塊假想的大陸,假定是用作平衡南半球。Over the past three million years, these regular changes in the amount of sunlight reaching the planet ' s surface have produced a long sequence of ice ages ( when great areas of northern hemisphere continents were covered with ice ) separated by short, warm interglacial periods
過去300萬年間,陽光抵達地表的規律變化造就了一系列的冰期(北半球陸地大部份都由冰覆蓋) ,間隔著短暫、溫暖的間冰期。The paper identifies the drought and flood years for precipitation during jja in global land, northern hemisphere, southern hemisphere and six continent areas respectively, and make statistic tests
劃分了全球、北半球、南半球和歐亞大陸、非洲、澳洲、北美、南美及南極大陸等大尺度區域的6 - 8月旱澇年並作了檢驗。In east asia, by the west pacific ocean
中國位於東半球,亞歐大陸的東部,太平洋的西岸。分享友人