欢迎访问《生态学杂志》官方网站,今天是 分享到:

生态学杂志 ›› 2011, Vol. 30 ›› Issue (02): 215-220.

• 研究报告 • 上一篇    下一篇

青海高原植被净初级生产力变化规律及其未来变化趋势

李红梅1周秉荣2**李 林1王振宇1   

  1. 1青海省气候中心,西宁 810001;2青海省气象科学研究所,西宁 810001
  • 出版日期:2011-02-08 发布日期:2011-02-08

Change pattern and its future trend of vegetation net primary productivity on Qinghai Plateau.

LI Hong-mei1, ZHOU Bing-rong2**, LI Lin1, WANG Zhen-yu1   

  1. 1Qinghai Climate Center, Xining 810001, China|2Institute of Meteorological Science of Qinghai Province, Xining 810001, China
  • Online:2011-02-08 Published:2011-02-08

摘要: 利用青海省43个气象台站1961—2009年的气象资料、22个样点生物量资料以及未来SRES A1B情景下的气象数据,验证了周广胜模型在青海地区的适用性,并根据此模型,计算了青海省1961—2009年及2020年、2050年和2080年NPP变化趋势。结果表明:周广胜模型所计算出的NPP值与实测值具有很好的相关性,此模型在青海高原具有一定的适用性;1961—2009年青海省平均NPP呈增加的趋势,趋势系数为0.067 t·hm-2·10 a-1,各地NPP变化趋势不尽相同,趋势系数为0.006~0.147 t·hm-2·10 a-1,其中柴达木盆地东部NPP增加趋势最明显,趋势系数为0.077~0.147 t·hm-2·10 a-1,果洛大部分地区NPP增加较小,趋势系数为0.006~0.030 t·hm-2·10 a-1;在气候变暖背景下,降水量和温度均与NPP存在较高的相关性,但降水量对NPP的影响效应大于温度;未来100年NPP变化趋势系数大致呈由东向西逐渐减小的趋势,青海东部地区NPP增加最为明显,为1.35~1.49 t·hm-2·100 a-1,青海西北部尤其是柴达木盆地和三江源区的部分地区NPP变化系数较小,为0.59~0.73 t·hm-2·100 a-1;2020年青海省NPP为2.5~7.0 t·hm-2·a-1,2050年NPP为2.7~7.5 t·hm-2·a-1,2080年NPP为2.9~7.8 t·hm-2·a-1

关键词: 羊草草甸草原, 热值, 能量积累和分配

Abstract: Based on the 1961-2009 meteorological data from 43 stations and the biomass data from 22 observation points in Qinghai Province as well as the future meteorological data estimated under SRES A1B scenario, this paper verified the applicability of Zhou Guang-sheng’s Model in the province, and, by using this model, calculated the vegetation net primary productivity (NPP) on Qinghai Plateau in 1961-2009, 2020s, 2050s, and 2080s. There was a very good correlation between the calculated and measured NPP values, suggesting the good applicability of Zhou’s Model in the province. In 1961-2009, the mean provincial vegetation NPP had an increasing trend, with an increment of 0.067 t·hm-2·10a-1, and the regional vegetation NPP varied greatly, with an increment of 0.077-0.147 t·hm-2·10 a-1 in eastern Chaidamu Basin and of 0.006-0.030 t·hm-2·10 a-1 in most areas of Guoluo. Under the background of climate warming, both the precipitation and the temperature had higher correlations with the NPP, but the influence of precipitation was bigger than that of temperature. In the coming 100 years, the increment of the NPP would be decreased gradually from east to west Qinghai, being 1.35-1.49 t·hm-2·100 a-1 in east Qinghai and 0.59-0.73 t·hm-2·100 a-1 in west Qinghai, especially in Chaidamu Basin and Three-River Source Area. In 2020s, 2050s, and 2080s, the vegetation NPP in Qinghai Province would have an increment of 2.5-7.0, 2.7-7.5, and 2.9-7.8 t·hm-2·a-1, respectively.

Key words: Aneurolepidium chinense grassland, Calorific value, Energy accumulation and allocation