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陕西省油松林生产力动态及对未来气候变化的响应
引用本文:霍晓英,彭守璋,任婧宇,曹扬,陈云明. 陕西省油松林生产力动态及对未来气候变化的响应[J]. 应用生态学报, 2018, 29(2): 412-420. DOI: 10.13287/j.1001-9332.201802.006
作者姓名:霍晓英  彭守璋  任婧宇  曹扬  陈云明
作者单位:1.西北农林科技大学水土保持研究所, 陕西杨凌 712100;2.西北农林科技大学黄土高原土壤侵蚀与旱地农业国家重点实验室, 陕西杨凌 712100;3.中国科学院水利部水土保持研究所, 陕西杨凌 712100
基金项目:本文由中央高校基本科研业务费专项资金项目(2452017183)、国家自然科学基金项目(41601058)、公益性行业(气象)科研专项(重大专项) (GYHY201506001-3)和中国科学院西部之光项目(XAB2015B07)资助
摘    要:本研究利用LPJ-GUESS模型,分析了陕西省油松林在未来时期(2015-2100年)不同气候情景下净初级生产力(NPP)的变化趋势.结果表明: 在未来时期,研究区温度在RCP2.6、RCP4.5和RCP8.5情景下将分别以0.12、0.23和0.54 ℃·10 a-1的速率显著升高;降水在RCP2.6和RCP8.5情景下无显著变化,在RCP4.5情景下将以14.36 mm·10 a-1的速率显著增加.与历史时期(1961-1990年)相比,研究区油松林的NPP在未来时期将升高1.6%~29.6%;在RCP8.5情景下21世纪末期(2071-2100年)油松林NPP将会升高45.4%;不同情景下油松林NPP表现为RCP8.5>RCP4.5>RCP2.6.在未来时期,陕北地区油松林NPP在RCP2.6和RCP4.5情景下将分别以41.00和21.00 g C·m-2·10 a-1的速率下降,该区油松林有变为碳源的可能.

关 键 词:气候变化  LPJ-GUESS模型  油松  净初级生产力  
收稿时间:2017-07-10

Dynamic change of Pinus tabuliformis forest productivity and its response to future climate change in Shaanxi Province,China.
HUO Xiao-ying,PENG Shou-zhang,REN Jing-yu,CAO Yang,CHEN Yun-ming. Dynamic change of Pinus tabuliformis forest productivity and its response to future climate change in Shaanxi Province,China.[J]. The journal of applied ecology, 2018, 29(2): 412-420. DOI: 10.13287/j.1001-9332.201802.006
Authors:HUO Xiao-ying  PENG Shou-zhang  REN Jing-yu  CAO Yang  CHEN Yun-ming
Affiliation:1.Institute of Soil and Water Conservation, Northwest A&F University, Yangling 712100, Shaanxi, China;2.Stake Key Laboratory of Soil Erosion and Dryland Farming on Loess Plateau, Northwest A&F University, Yangling 712100, Shaanxi, China;3.Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling 712100, Shaanxi, China
Abstract:This study analyzed the dynamics of net primary productivity (NPP) of Pinus tabuliformis forest under future climate scenarios in Shaanxi Province during 2015-2100, using a dynamic vegetation model (LPJ-GUESS). The results showed that in the 2015-2100 period, annual mean temperature of this region would significantly increase by 0.12, 0.23 and 0.54 ℃·10 a-1 under RCP2.6, RCP4.5 and RCP8.5 scenarios, respectively, while the annual precipitation would have no significant change under climate scenarios except RCP4.5, under which it would significantly increase by 14.36 mm·10 a-1. Compared with the NPP of P. tabuliformis forest in the historical period (1961-1990), it would increase by 1.6%-29.6% in the future period, and the enhancement could reach 45.4% at the end of this century (2071-2100) under RCP8.5 scenario. The NPP under the RCP8.5 scenario was the highest, followed by the RCP4.5 and RCP2.6 scenarios. During 2015-2100, the NPP in the northern Shaanxi region would significantly decrease with the rate of 41.00 and 21.00 g C·m-2·10 a-1 under the RCP2.6 and RCP4.5 scenarios, respectively, implying that this area has the potentiality to be carbon source.
Keywords:Pinus tabuliformis  LPJ-GUESS model  climate change.  net primary productivity  
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