latitude of observation 中文意思是什麼

latitude of observation 解釋
觀測點緯度
  • latitude : n 1 緯度 (opp longitude)。2 【天文學】黃緯。3 〈pl 〉 (以緯度而論的)地區,地方,地域。4 (見...
  • of : OF =Old French 古法語。
  • observation : n 1 觀察,注意;觀察力;?望。2 觀測,實測;【航海】測天;【軍事】觀測,監視,偵察。3 (觀察得的)...
  1. Of sept. when, in the manner as above said, i first set foot upon this horrid island, when the sun being, to us, in its autumnal equinox, was almost just over my head, for i reckon d my self, by observation, to be in the latitude of 9 degrees 22 minutes north of the line

    我估計,我是九月三十日踏上這可怕的海島的當時剛入秋分,太陽差不多正在我頭頂上。所以,據我觀察,我在北緯九度二十二分的地方。
  2. In this distress, we had besides the terror of the storm, one of our men dyed of the calenture, and one man and the boy wash d over board ; about the 12th day the weather abating a little, the master made an observation as well as he could, and found that he was in about 11 degrees north latitude, but that he was 22 degrees of longitude difference west from cape st. augustino ; so that he found he was gotten upon the coast of guinea, or the north part of brasil, beyond the river amozones, toward that of the river oronoque, commonly call d the great river, and began to consult with me what course he should take, for the ship leaky and very much disabled, and he was going directly back to the coast of brasil

    在這危急的情況下,風暴已使我們驚恐萬狀,而這時船上一個人又患熱帶病死去,還有一個人和那個小傭人被大浪卷到海里去了。到第二十二天,風浪稍息船長盡其所能進行了觀察,發現我們的船已刮到北緯十一度左右的地方,但在聖奧古斯丁角以西二十二經度。船長發現,我們的船現在所處的位置在巴西北部或蓋亞那海岸我們已經駛過了亞馬孫河的入海口,靠近那條號稱"大河"的俄利諾科河了。
  3. There is no perspicuity verge between the west and the east of qinling mountains, so we have to draw a line to divide it into two parts. by analyzing the chang of observation spot " s precipitation in summer and in autumn on the same latitude, we can make a conclusion that 108 ewill be the line possibly. the paper was going on under the background of global chang by compairing the variation characteristics of norm annual air temperature and norm annual precipitation, and by compairing air temperature and precipitation over the season,

    秦嶺東部地區氣候變化總體趨勢為降水減少、氣溫遞增,其中近50年的時間里,氣溫共遞增0 . 185 ,同時降水減少75 . 35mm ,表現為暖干化特點,其暖化的特點表現在冬半年的暖冬尤其是冬季增溫強烈,干化則主要集中在夏季降水的銳減;而秦嶺西部地區則降水減少的同111氣溫下降,近50年來,氣溫共下降0
  4. Results of recent observation and numerical experiments show that prominent difference exists between air - sea interaction in tropical and in mid - latitude, and work is not enough related to the impact of persistent ssta on the circulation considering different district in pacific

    觀測分析和數值模擬結果表明中緯度與熱帶地區的海氣相互作用存在差異,但深入討論不同關鍵海區的持續性ssta對大氣環流影響的工作還不充分。
  5. But as i had no instruments to take an observation to know what latitude we were in, and did not exactly know, or at least remember what latitude they were in ; i knew not where to look for them, or when to stand off to sea towards them ; otherwise i might now easily have found some of these islands

    過去我曾到這一帶的海岸來過一次,知道加那利群島和維德角群島離大陸海岸不遠。但船上沒有儀器,無法測量我們所在地點的緯度,而且,我也已不記得這些群島確切的緯度了,因此也無法找到這些群島,也不知道什麼時候該離開海岸,駛向海島。
  6. The simulated results are consistent with the observation, and the feature of sst ' s variation as a function of latitude ( longitude ) is well reproduced

    模式較好地模擬出了平均海溫的經向分佈與緯向分佈情況,結果與觀測基本相符。
  7. In this paper, the solar and land - atmosphere radiation rates are calculated by modtran3 model and satellite observation as well as surface data, solar direct irradiance infrared irradiance solar heating rate and infrared cooling rate were calculated from 43 samples of sunshine day and 5 samples of cloudy day 3 samples of rainy day of different latitudes in 12 stations. the paper analyzed solar heating rate and infrared cooling rate in sunshine day, the factors such as zenith angle, water vapor and latitude were found out correlating with solar heating rate and infrared cooling rate. solar heating rate and infrared cooling rate change on the same day and at the same station

    在對晴空大氣的計算中,本文對太陽的直接輻射與地氣系統的紅外輻射狀況進行了分析,並討論在不同的大氣狀況下太陽加熱率和紅外冷卻率的情況,找出與太陽加熱率和紅外冷卻率變化相關較大的因子?太陽天頂角和水汽條件、緯度;本文還進一步分析了不同緯度樣本的太陽加熱率與紅外冷卻率日變化及有雲、有雨情況下太陽加熱率和紅外冷卻率的變化情況:另外,文中通過改變二氧化碳在大氣中含量的方法,討論了它對太陽加熱率與紅外冷卻率的影響。
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