[1]周礼华,黄 力,钱深华,等.金佛山西坡气温的垂直变化特征[J].山地学报,2019,(6):818-827.[doi:10.16089/j.cnki.1008-2786.000472]
　ZHOU Lihua,HUANG Li,QIAN Shenhua,et al.Vertical Change in Air Temperature on the West Slope of Mt. Jinfo, China[J].Mountain Research,2019,(6):818-827.[doi:10.16089/j.cnki.1008-2786.000472]
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金佛山西坡气温的垂直变化特征()
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2019年第6期
页码:
818-827
栏目:
山地环境
出版日期:
2019-11-30

文章信息/Info

Title:
Vertical Change in Air Temperature on the West Slope of Mt. Jinfo, China
文章编号:
1008-2786-(2019)6-818-10
作者:
周礼华1; 黄 力1; 钱深华1; 李 莉2*; 杨永川1
1.重庆大学 三峡库区生态环境教育部重点实验室,重庆 400045; 2.重庆大学 建筑城规学院,重庆 400030
Author(s):
ZHOU Lihua1;  HUANG Li1;  QIAN Shenhua1;  LI Li2*;  YANG Yongchuan1
1. Key Laboratory of Three Gorges Reservoir Region Eco-Environment of Ministry of Education, Chongqing University, Chongqing 400045, China; 2. Faculty of Architecture and Urban Planning, Chongqing University, Chongqing 400030, China
关键词:
垂直变化;  气温直减率;  金佛山;  重庆
Keywords:
vertical change;  temperature lapse rate;  Mt. Jinfo;  Chongqing
分类号:
P423.3~A
DOI:
10.16089/j.cnki.1008-2786.000472
摘要:
山地气温的实测数据是相关学科极其重要的基础资料,其垂直变化特征是研究山地气温的重要内容之一。本研究使用HOBO Onset自动温度记录仪于2017年6月-2018年6月对重庆金佛山西坡14个海拔高度的气温进行30 min间隔的连续监测,分析了金佛山西坡气温的时序差异和垂直变化规律。结果如下:(1)金佛山西坡年平均气温直减率为0.53 ℃/100 m,气温直减率的月份间差异较小;(2)平均最高气温、平均最低气温及年平均气温随海拔升高而线性降低,极端高温沿海拔梯度的变化不明显;(3)月平均日较差随海拔升高呈二次曲线变化;(4)日平均气温≥0 ℃、≥5 ℃和≥10 ℃的积温随海拔升高而降低,积温递减率几乎相同(约184.2 ℃/100 m),相应积温持续天数随海拔升高以平均5 d/100 m的速率递减;(5)各监测点实测气温较气温地理分布模型求得的气温值偏小,而较基于WorldClim数据库所得的插值气温整体偏大。
Abstract:
The temperature records measured in mountains serve as basic data for scientific support of related disciplines, and for years the concern about the altitude variation in mountain temperature have grown in mountain researchers. Jinfo Mountain is the main peak of the Dalou Mountains, Yunnan-Kweichow Plateau, China, and it is a major component of Southern China Karst World Heritage, featured by important ecological value. In this study, it installed 14 sets of HOBO Onset micro climatic recorders on the west slope of Mt. Jinfo and had recorded continuously the temperature in 30min intervals at 14 sites from June 2017 to June 2018. And based on this, it analyzed the temporal difference and vertical variation of temperature on the west slope of Mt. Jinfo. The results showed that:(1)The annual average temperature lapse rate on the west slope of Mt. Jinfo was 0.53 ℃/100 m, with minor difference between months;(2)The average maximum temperature, average minimum temperature, and annual average temperature all decreased linearly with increasing altitude, while the extreme-high temperature did not change significantly along the elevational gradient;(3)The monthly mean daily range varied with elevation in a quadratic curve;(4)The accumulated temperature of ≥0 ℃, ≥5 ℃, and ≥10 ℃ all decreased linearly with increasing altitude, with a decreasing rate of accumulated temperature almost the same(approximately 184.2 ℃/100 m), and the corresponding duration for accumulated temperature continued to decrease by 5d for per 100 m increase in elevation;(5)Compared with the measured temperature in-situ, the calculated temperature based on the temperature geographical distribution model was higher at each monitoring site, while the interpolated temperature based on WorldClim database was lower as a whole.

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备注/Memo

备注/Memo:
收稿日期(Received date):2019-04-27; 改回日期(Accepted date):2019-12-10
基金项目(Foundation item):重庆市自然科学基金项目(CSTC2016jcyjA0379)。 [Natural Science Foundation of Chongqing, China(CSTC2016jcyjA0379)]
作者简介(Biography):周礼华(1992-),男,硕士研究生,主要研究方向:植被生态学。[ZHOU Lihua(1992-), male, M.Sc. candidate, research on vegetation ecology] E-mail: lhzhou1023@163.com
更新日期/Last Update: 2019-11-30