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环青海湖地区草地近地层气象要素变化特征
引用本文:朱宝文,宋理明,许存平,姜朝阳,马宗泰,周华坤,徐有绪. 环青海湖地区草地近地层气象要素变化特征[J]. 中国农业气象, 2007, 28(4): 389-392
作者姓名:朱宝文  宋理明  许存平  姜朝阳  马宗泰  周华坤  徐有绪
作者单位:1. 青海省海北牧业气象试验站,西海镇,810200
2. 青海省海北州气象局
3. 中国气象科学研究院
4. 中国科学院西北高原生物研究所
基金项目:中国气象局资助项目;中国科学院知识创新工程项目;国家自然科学基金;国家科技支撑课题
摘    要:利用青海湖北岸海北牧业气象试验站2006年5月-12月观测的天然草地近地面层气象要素梯度资料,分析了该地区近地层温度、湿度和风速的日变化规律及其廓线特征。结果表明:青海湖北岸草地近地层0.3—10.0m高度范围内温度、相对湿度和风速都呈现出明显的以24h为周期的日变化规律;各层温度最高和最低时的位相随高度增加而滞后,相对湿度和风速最大与最小时的位相随高度增加而提前;14时温度随高度的增加而降低,20时的温度随高度增加先增后降,温度廓线在4.0m高度存在一拐点,随后逐渐进入逆温状态,至8时逆温程度达到最大;不论白天还是夜间,相对湿度随高度的增加而减小;风速随高度的增加而增大。

关 键 词:气象要素  日变化  廓线特征  近地层
修稿时间:2007-04-08

Characteristics of Changes of Micro-Meteorology in Surface Layer of Grassland in Regions around Qinghai Lake
ZHU Bao-wen,SONG Li-ming,XU Cun-ping,JIANG Chao-yang,MA Zong-tai,ZHOU Hua-kun,XU You-xu. Characteristics of Changes of Micro-Meteorology in Surface Layer of Grassland in Regions around Qinghai Lake[J]. Chinese Journal of Agrometeorology, 2007, 28(4): 389-392
Authors:ZHU Bao-wen  SONG Li-ming  XU Cun-ping  JIANG Chao-yang  MA Zong-tai  ZHOU Hua-kun  XU You-xu
Affiliation:1. Haibei Animal Husbandry Meteorological Experimental Station of Qinghai Province,Xihai 810200, China; 2. Meteorological Administration of Haibei state ; 3. Chinese Academy of Meteorological Sciences ; g. Northwest Institute of Plateau Biology, CAS
Abstract:Based on the meteorological data in the surface layer of grassland in the north shore of Qinghai Lake from May to December in 2006 observed by Haibei Animal Husbandry Meteorological Experimental Station, the characteristics of changes of the diurnal variation and the vertical profiles of the wind speed, temperature and humidity were investigated. The results showed that the wind speed, temperature and relative humidity showed an obvious diurnal variation above 0.3m and below 10m in the surface layer of grassland in the north shore of Qinghai Lake. The phase of the maximum and minimum temperature delayed with the increase of the height and the phase of the maximum and minimum relative humidity and wind speed advanced with the increase of the height. The temperature at fourteen o'clock decreased with the increase of the height and the temperature at twenty o'clock increases first and decreased later with the increase of the height. The temperature profiles had an inflexion at the height of 4m, then into the status of the inversion. The degree of the inversion reached biggest at eight o'clock. Relative humidity decreased and wind speed increased with the increase of the height whenever day and night.
Keywords:Meteorological factors  Diurnal variation  Characteristics of profiles  Surface layer
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