上高原 meaning in Chinese
hauts plat
Examples
- In order to cultivate the kalgan mushroom that originated in grass land of zhangjiakou in south of shijihuazhuang , we studied the ratio of the material which used for cultivating the kalgan mushroom
摘要褐蘑菇产自内蒙和冀北坝上高原，将它南移下坝进行人工栽培是本研究的目的。 - Therefore , in order to maintain the ecological balance of bashang plateau and promote the development of local agriculture , forestry and animal husbandry , it is necessary to make reasonable adjustments to the land utilization
因此，要维护坝上高原的生态平衡，促进当地农林牧生产的发展，必须对土地利用进行合理调整。 - Based on the analysis of remote sensing data of different stages of hebei bashang plateau area , the author thinks that the changes of the plateau ecological environment are caused by the changes of the land utilization condition
摘要通过对河北省坝上高原地区不同时期的遥感资料进行分析，认为引起坝上高原生态环境变化的原因是土地利用状况的变化。 - By using ncep / ncar reanalysis data of height and wind , the inter - monthly lpac map , the climate lapc map , inter - annual anomaly map and mean variance map of monthly wind field of 850 and 500hpa and monthly height field of 850 , 500 , 150 , 30hpa are calculated in a globe - belt area , which situates between 30 s and 75 n , from december 1957 to december 1997 , according them we analysis the rule of the season transfer and anomaly of nh mean circulation . the results show that the climate map of lapc can describe the seasonal transfer process of large scale circulation better . the advance process of summer circulation establish is form south to north at the middle and lower level of the troposphere , that is reflected primly in the inter - monthly wind and pressure map of lapc ; at lower lever of stratosphere , the establish process is simulate to that of troposphere , and reflect of process of that the south asia high toward plateau ; at middle stratosphere the summer circulation establish begins at middle and high latitude initially , and then transmits to low latitude gradually , while the seasonal variability in mid - stratosphere is stronger than it in troposphere and low - stratosphere
利用ncep ncar再分析高度场和风场资料，计算了30 s 75 n球带区域1957年12月至1997年12月逐月850 、 500hpa风场及850 、 500 、 150 、 30hpa高度场月际局地型相似系数图、多年平均图(即气候lpac图) 、年际异常图及均方差图，在此基础上，分析了北半球平均环流季节转换及其异常的规律。分析表明，气候局地型相似系数图较好地给出了大尺度环流季节转换发生的过程：在对流层中、下部，风、压场月际局地型相似系数图清楚地反映了夏季型环流建立由南向北的推进过程；低平流层夏季型环流的建立与对流层接近，其中，南亚高压上高原过程有明显反映：中平流层，夏季型环流的建立明显表现为从中、高纬度开始，逐步向低纬传播的特征，且变化较对流层和低平流层明显。 - Monthly average composite potential geographical high in nine levels ( 850hpa , 700hpa , 600hpa , 500hpa , 200hpa , 100hpa , 70hpa , 50hpa , 30hpa ) are studied , and we also study the composite potential geographical high ' s similarity between 500hpa and other eight levels . all the studies show that the drought flow pattern " west positive east negative " and flood flow pattern " west negative east positive " not only exist in 500hpa presented in 80s last century , but also exist in other levels
并计算了500hpa合成高度场与其余8个层次合成高度场旱、涝流型的相似性度量，结果表明：上世纪八十年代提出的500hpa层次上高原东北侧“西正东负” (或“西高东低” )少雨流型及“西负东正” (或“西低东高” )多雨流型的特征，在850hpa 70hpa整层大气中仍然存在。