干旱区生态环境知识资源中心(Arid): 19802014年中亚地区植被净初级生产力对气候和CO

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	19802014年中亚地区植被净初级生产力对气候和CO_2变化的响应
其他题名	The Responses of the Net Primary Productivity of the Dryland Ecosystems in Central Asia to the CO_2 and Climate Changes during the Past 35 Years
	朱士华 1; 艳燕 2; 邵华 2; 李超凡 2
来源期刊	自然资源学报
ISSN	1000-3037
出版年	2017
卷号	32 期号:11 页码:1844-1856
中文摘要	中亚干旱区分布着世界80%以上的温带荒漠,受气候变化影响显著。论文首先收集实验观测数据验证了干旱区生态系统模型(AEM),然后运用AEM开展数值模拟实验量化研究了19802014年中亚净初级生产力(NPP)的时空格局,评估了不同环境因子(降水、温度、CO_2)的相对贡献率及其交互效应。结果表明:过去35 a中亚干旱区年均NPP总量为1 125129 Tg C (1 T=10~(12))或21825g C/m~2。哈萨克斯坦北部地区年NPP值较高(34939 g C/m~2),而南疆地区年NPP值较低(12345 g C/m~2)。19802014年间,中亚NPP总体呈减少趋势[-0.71 gC/(m~2·a)],南疆极端干旱区的NPP降低最为显著[-2.05 g C/(m~2·a)]。相较于19801984年NPP均值,在19852014年中亚区域NPP总体降低了118 Tg(-10%)。其中CO_2施肥效应促进NPP增加了99.7 Tg (+8%),气温升高的正效应促进NPP增加了35.4 Tg(+2%),而降水减少导致NPP降低了221 Tg(-18%)。研究区内9%的地区的NPP主要控制因子为温度,主要分布在天山和哈萨克斯坦北部等高纬高寒地区。降水主控区面积占整个研究区的69%,主要分布在荒漠平原特别是南疆等植被受水分限制的区域。CO_2主控区占研究区面积的20%,主要分布在天山中山带森林区和低海拔地区等水热条件好的区域。研究表明新疆南部地区是中亚的关键生态脆弱区,其生态安全面临着气候变化的挑战,但21世纪的升温不大可能因刺激自养呼吸而对中亚区域NPP造成显著影响。
英文摘要	More than 80% of world,s temperate desert locates in Central Asia, dryland that experienced strong warming and significant changes in precipitation pattern in recent decades. The objectives of this study was to quantify spatio-temporal patterns of net primary productivity in Central Asia over the past 35 years, and investigate the relative contribution and interactive effect of climate controls including temperature, precipitation and CO_2, using the Arid Ecosystem Model (AEM), which performed well in predicting the dryland ecosystems’ responses to climate changes according to our evaluation. The results show the 35- year averaged annual NPP of Central Asia amounted to 1 125129 Tg C/a (1 T=10~(12)),or 21824 g C/(m~2 · a), with an overall declining trend of 0.71 g C/(m~2 · a). The northern Kazakhstan had relatively high NPP of 34939 g C/(m~2 · a), while the southern Xinjiang of China had relatively low NPP of 12345 g C/(m~2 · a). During the last 35 years, the NPP of the southern Xinjiang subregion declined significantly with a trend of -2.05 g C/(m~2 · a). Comparing the NPP during 1985-2014 to the NPP during 1980-1984,we found the regional NPP decreased 118 Tg or 10%,with positive contribution of 35.4 Tg or + 2% from temperature change, positive contribution of 99.7 Tg or +8% from CO_2 change, negative contribution of 221 Tg or-18% from precipitation change. The temperature was the dominant factor on NPP in 9% of the study area, mainly in the Tianshan Mountains and northern Kazakhstan, where the temperature increased by 0.03 ℃/a during 1980-2014. Precipitation was the dominant factor on NPP in 69% of the study area, mainly in the desert subregion and the dryland of southern Xinjiang of China, where the vegetation was limited by water. CO_2 was the dominant factor on NPP in 20% of the study area, mainly in the lower altitude regions of Tianshan Mountains, where the hydrothermal condition was suitable for vegetation growth. This study shows that the southern Xinjiang of China is the fragile eco-environmental subregion in Central Asia, whose ecosystem security is facing the challenges of climate change. However, increasing temperature is unlikely to stimulate autotrophic respiration and cause a significant impact on regional NPP in Central Asia.
中文关键词	中亚AEM模型 ; 干旱区气候变化
英文关键词	NPP Central Asia arid ecosystem model NPP dryland climate change
语种	中文
国家	中国
收录类别	CSCD
WOS类目	PLANT SCIENCES
WOS研究方向	Plant Sciences
CSCD记录号	CSCD:6110240
来源机构	中国科学院新疆生态与地理研究所
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/237256
作者单位	1.南京大学国际地球系统科学研究所, 荒漠与绿洲生态国家重点实验室, 南京, 江苏 210093, 中国; 2.中国科学院新疆生态与地理研究所, 荒漠与绿洲生态国家重点实验室, 乌鲁木齐, 新疆 830011, 中国
推荐引用方式 GB/T 7714	朱士华,艳燕,邵华,等. 19802014年中亚地区植被净初级生产力对气候和CO_2变化的响应[J]. 中国科学院新疆生态与地理研究所,2017,32(11):1844-1856.
APA	朱士华,艳燕,邵华,&李超凡.(2017).19802014年中亚地区植被净初级生产力对气候和CO_2变化的响应.自然资源学报,32(11),1844-1856.
MLA	朱士华,et al."19802014年中亚地区植被净初级生产力对气候和CO_2变化的响应".自然资源学报 32.11(2017):1844-1856.