本报告基于祁连山“山水林田湖草沙”系统的“天地空”一体化监测系统的综合监测数据集,开展了1985~2020年祁连山“山水林田湖草沙”系统生态功能动态变化评估。主要评估结果包括:(1)泛祁连山区综合动态度为0。07%,祁连山区为0。13%、国家公园为0。21%;与1985年相比,2020年泛祁连山区的冰/雪面积缩减42%,水体面积增长约23%,其他生态系统面积略有增长,“林田湖草”比例略有变化,主要原因为水体面积增加。(2)1985~2020年,泛祁连山区除林地外各生态系统NPP呈显著增加趋势,按增长速率大小依次为湿地、灌丛、草地、裸地和耕地,林地NPP呈显著减少趋势,该区多年NPP均值约为67gCm-2a-1;泛祁连山区中,青海湖流域和大通河—湟水流域NPP变化趋势不显著,其他流域呈显著增加趋势;祁连山区和国家公园NPP呈显著增加趋势,其中,祁连山区2400~3300m和国家公园2400~3200m的林地NPP呈显著减少趋势。(3)泛祁连山区、祁连山区和国家公园固碳量呈波动上升趋势,祁连山区与国家公园以草地固碳为主。(4)以黑河上游为中心的山区降雨量占全区的55。5%、蒸散量占49。3%、径流量占87。8%、产水量占66。4%,在整个区域水源涵养中具有主导作用,山区以高寒草甸和高寒草原为主的草地是水源涵养的主要生态系统。1985~2010年,祁连山区水源涵养各分量波动上升,2010年起有下降趋势。上述研究结果为系统深入认识祁连山“山水林田湖草沙”系统生态功能现状提供了科学依据和数据支撑,并可服务于泛第三极的绿色发展。
<<The Qilian Mountain is an important ecological security barrier in western China,and also an important water source for the Yellow River and many inland rivers. The assessment on dynamic change of ecological functions in the Qilian Mountain’s mountain-river-forest-field-lake-grassland-desert system in 1985-2020 is carried out based on the comprehensive monitoring data set of the sky-ground integrated monitoring system. Main findings of assessment are as follows:(1)The combined dynamic degree is 0.07%,0.13%,and 0.21% in the pan-Qilian-Mountain region,the Qilian Mountain,and the Qilian Mountains National Park respectively;in 2020,the area of ice/water has shrunk by 42%,the water area has increased by about 23%,the area of other ecosystems has increased slightly,and the proportion of forest,field,lake and grass has changed slightly mainly due to the increase in the water area,compared with 1985;(2)over 35 years,NPP of all ecosystems,except for woodland,in the pan-Qilian-Mountain region has showed a significant increasing trend,with NPP of ecosystems for wetland,scrubland,grassland,bare land and arable land sequenced in order of growth rate,while NPP of woodland has showed a significant decreasing trend,with the average value of multi-year NPP in the region being about 67 gCm-2a-1;in the pan-Qilian-Mountain region,NPP of Qinghai Lake basin and Datong River-Huangshui River basin has showed a insignificant variation trend,while NPP of other basins has showed a significant increasing trend;NPP in the Qilian Mountain region and the Qilian Mountains National Park has showed a significant increasing trend,among which,the woodland NPP in the Qilian Mountain region at 2400-3300 m and the Qilian Mountains National Park at 2400-3200 m has showed a significant decreasing trend;(3)the carbon sequestration in the pan-Qilian-Mountain region,the Qilian Mountain region,and the Qilian Mountains National Park has showed a fluctuating upward trend,of which the carbon sequestration in the Qilian Mountain region and the Qilian Mountains National Park has been dominated by grassland carbon sequestration;(4)the precipitation in the mountainous area centered on the upper reaches of the Heihe River has accounted for 55.5% of the regional sum,with evapotrans-piration accounting for 49.3%,runoff accounting for 87.8%,and water production accounting for 66.4%. The mountainous area has a dominant role in the water conservation of the whole region,in which the grasslands dominated by alpine meadows and alpine grasslands are the main ecosystem of water conservation. From 1985 to 2010,each component for water conservation of the Qilian Mountain has fluctuated and rose,and then showed a decreasing trend since 2010. The results of the above study provide scientific basis and data support for the systematic and in-depth understanding of the ecological functions of the Qilian Mountain’s mountain-river-forest-field-lake-grassland-desert system,and can serve the green development of the pan-third pole.
<<Keywords: | Qilian MountainSoil MoistureEvapotranspirationNet First ProductivityCarbon Sequestration Function |