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1.The results indicated that the LRGR mean winter rainfall longitudinally distributed along river, while the unique topography of LRGR did not obviously have impact on the winter rainfall; the winter temperature distribution was like belt, which decreased from low latitude to high latitude; the passing-obstructing effect of LRGR cannot be clearly showed with the winter temperature distribution; but such effect is obvious over Nu-valley and Lancang-valley.
结果表明:纵向岭谷区多年平均冬季降水空间上沿河流呈纵向分布;但纵向岭谷独特地形对冬季降水变化的空间分布影响不明显;冬季气候平均温度大致呈东西向带状分布,由低纬到高纬温度逐渐递减;在区域上,纵向岭谷独特地形的“通道-阻隔”作用对冬季温度空间分布的影响不明显;但在怒江和澜沧江流域,这种影响则较为明显。收藏指正
2.THE TIDAL EFFECT ON THE TIME AND LATITUDE OBSERVATION OF SHANGHAI OBSERVATORY
上海天文台天文时纬观测中的潮汐影响收藏指正
3.LATITUDINAL EFFECT OF MAGNETIC STORM ON APRIL 6,2000 AT LOW-LATITUDE MERIDIAN CHAIN
2000年4月6日磁暴期间磁扰变化在低纬子午链的纬度效应收藏指正
4.By using the Fourier method to solve the barotropic and nondivergent vor-ticity equation, the effect produced by the middle or low latitude disturbance to the flow field at the low or middle latitude is investigated.
用付里叶方法求解正压无辐散涡度方程,把初始扰动分别加在中纬或低纬,求得这些扰动在低纬或中纬度产生的作用。收藏指正
5.In the higher- latitude zones (40°S- 70°S,40°N- 70°N),the sea levels in both the northern - western andsouthern - western Pacific areas are being the obvious risings and their rates in the higher latitude zones are 1. 5 mm/yr and 2. 5 mm/yr, respectively, it is confirmed that the effect ofice - sheet melting in the Antarctica on the sea level change is stronger than that in theGreenland.
在高纬度区(40°S-70°S,40°N-70°N),西北和西南太平洋的海平面都呈现明显的上升趋势,其速率分别为1.5mm/yr和2.5mm/yr,这证实了南极洲冰盖的消融对海平面变化的影响要比格陵兰岛的强烈;收藏指正
6.Based on GIS technique and geographic correction model with 5 environmental factors of longitude,latitude,height above the level,grade and slope of terrain, drought spatial distribution with relative high resolution of 1 km was made from scatter data of DDI of 86 stations,which could reflect the effect of terrain factors to drought distribution with more detail.
借助G IS技术和包括经度、纬度、海拔、坡度、坡向5个环境因子的地理订正模型,对离散DD I资料进行1 km空间分辨率的精细化反演,能够清晰刻画地形、地貌对干旱程度空间分布的影响.收藏指正
7.These results suggest that altitude effect of foliar δ 13C was mainly ascribed to temperature and atmospheric pressure (the partial pressure of CO 2), while temperature and relative humidity were possibly responsible for the latitude and longitude trends of foliar δ 13C.
初步分析表明 ,大气压力 (CO2 分压 )和温度的协同变化导致了叶片δ13C值随着海拔变化的分布格局 ,而温度和相对湿度的变化是引起叶片δ13C值的经、纬度效应的主要因子 .收藏指正
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