中国农业气象 ›› 2016, Vol. 37 ›› Issue (01): 11-18.doi: 10.3969/j.issn.1000-6362.2016.01.002

• 论文 • 上一篇    下一篇

温带针阔混交林内温度和水汽压垂直梯度变化特征

杨亚丽,任传友,王艳华,乔延艳,秦 瑜   

  1. 1. 沈阳农业大学农学院大气科学系,沈阳 110866;2. 辽宁省本溪市气象局,本溪 117000
  • 收稿日期:2015-05-19 出版日期:2016-02-20 发布日期:2016-02-24
  • 作者简介:杨亚丽(1989-),女,硕士生,主要从事应用气候学研究。E-mail:15040048856@126.com
  • 基金资助:

    国家自然科学基金(31070429;31201124)

Vertical Gradient Variations of Temperature and Vapor Pressure in Temperate Coniferous and Broad-leaved Mixed Forest

YANG Ya-li, REN Chuan-you, WANG Yan-hua, QIAO Yan-yan, QIN Yu   

  1. 1.College of Agriculture, Shenyang Agriculture University, Shenyang 110866,China; 2.Meteorological Bureau of Benxi, Benxi 117000
  • Received:2015-05-19 Online:2016-02-20 Published:2016-02-24

摘要:

应用长白山针阔混交林2003-2005年空气温度和水汽压梯度观测资料,以4、7、10和1月分别代表春、夏、秋和冬季,分析不同季节典型晴天条件下林内气温、水汽压的垂直分布规律及其日变化特征,以冠层顶部的气温和水汽压为本底值构建林内气温和水汽压随观测高度变化的廓线函数,分析其变化特征。结果表明:(1)林内各观测高度的气温均具有单峰曲线形式的日变化特征,最高值出现在15:00左右,最低值出现在日出前,林内各高度气温日较差以秋季最大,冬季最小,各季气温日较差均随高度的增加而减小;(2)在春、秋和冬季,林内气温表现出随高度增加而升高的趋势,且具有明显的日变化规律,在正午前后林内气温的垂直梯度较小,甚至表现出气温随高度增加而减小的趋势,而其它时刻林内气温的垂直梯度较大,在夏季,各个时刻林内气温均随观测高度的增加而升高;(3)不同季节林内水汽压的日变化特征不同,春、秋和冬季各观测高度水汽压皆呈单峰曲线的分布规律,而夏季则呈双峰曲线形式的日变化规律;(4)同一时刻不同季节林内水汽压垂直分布规律存在显著差异,而同一季节不同时刻的水汽压垂直分布廓线形状相似,夏季林内水汽压随观测高度增加而降低的规律明显,其它季节水汽压的垂直梯度则较小;(5)林内气温和水汽压垂直分布廓线均近似满足对数曲线规律。

关键词: 森林, 气温, 水汽压, 垂直梯度, 对数规律

Abstract:

Using the data of air temperature and vapor pressure observed at temperate coniferous and broad-leaved mixed forest ecosystem over Changbai mountain during 2003 to 2005, with April, July, October and January represented as spring, summer, autumn and winter, respectively, the vertical distribution patterns of them and their diurnal variations were analyzed on typical sunny days in four representative months, and the profile functions of air temperature and vapor pressure with observed height under the canopy top were constructed by method of using the top of canopy air temperature and water vapor pressure as normalized values. The results are as followed: (1)the diurnal variation of air temperature characterized by single peak curve obviously with the highest value at 15:00 and the lowest at dawn. The diurnal air temperature range decreased with higher height in all seasons and with the maximum diurnal air temperature range in autumn and minimum in winter. (2)In spring, autumn and winter, air temperature within forest increased as height ascended accompanied by obvious diurnal change pattern. The vertical gradient of air temperature was extremely large at times except noon, whereas the gradient was small and even showed the trend of air temperature decreasing as height ascended at noon. In summer, air temperature increased with observed height higher at any times. (3)The diurnal variations of the vapor pressure were different in four seasons. The vapor pressure showed diurnal patterns by single peak curve in spring, autumn and winter contract with that by double peak curve in summer. (4)The vertical distribution of vapor pressure at given time was seasonal divergence obviously, whereas at given season they had the similar vertical distribution at different times. The vertical gradient of vapor pressure was larger in summer than that in other seasons characterized by vapor pressure went down with observed height higher. (5)The profiles of air temperature and vapor pressure within forest can be fitted with logarithm law.

Key words: Forest, Air temperature, Vapor pressure, Vertical gradient, Logarithm law