Using the Integrated Biosphere Simulator, a dynamic vegetation model, this study initially simulated the net primary productivity（NPP） dynamics of China＇s potential vegetation in the past 55 years（1961–2015） and...Using the Integrated Biosphere Simulator, a dynamic vegetation model, this study initially simulated the net primary productivity（NPP） dynamics of China＇s potential vegetation in the past 55 years（1961–2015） and in the future 35 years（2016–2050）. Then, taking the NPP of the potential vegetation in average climate conditions during 1986–2005 as the basis for evaluation, this study examined whether the potential vegetation adapts to climate change or not. Meanwhile, the degree of inadaptability was evaluated. Finally, the NPP vulnerability of the potential vegetation was evaluated by synthesizing the frequency and degrees of inadaptability to climate change. In the past 55 years, the NPP of desert ecosystems in the south of the Tianshan Mountains and grassland ecosystems in the north of China and in western Tibetan Plateau was prone to the effect of climate change. The NPP of most forest ecosystems was not prone to the influence of climate change. The low NPP vulnerability to climate change of the evergreen broad-leaved and coniferous forests was observed. Furthermore, the NPP of the desert ecosystems in the north of the Tianshan Mountains and grassland ecosystems in the central and eastern Tibetan Plateau also had low vulnerability to climate change. In the next 35 years, the NPP vulnerability to climate change would reduce the forest–steppe in the Songliao Plain, the deciduous broad-leaved forests in the warm temperate zone, and the alpine steppe in the central and western Tibetan Plateau. The NPP vulnerability would significantly increase of the temperate desert in the Junggar Basin and the alpine desert in the Kunlun Mountains. The NPP vulnerability of the subtropical evergreen broad-leaved forests would also increase. The area of the regions with increased vulnerability would account for 27.5% of China.展开更多
【目的】定量评估半干旱牧区天然打草场的生产能力,分析天然打草场的退化程度,明确气候因子对打草场生长过程的影响。【方法】利用Miami和Tharnthwaite Memorial模型计算2000—2017年半干旱牧区天然打草场气候生产潜力,并结合近18年的...【目的】定量评估半干旱牧区天然打草场的生产能力,分析天然打草场的退化程度,明确气候因子对打草场生长过程的影响。【方法】利用Miami和Tharnthwaite Memorial模型计算2000—2017年半干旱牧区天然打草场气候生产潜力,并结合近18年的中分辨率成像光谱仪(MODIS)净初级生产力(NPP)产品(MOD17A2H)进行分析。【结果】2000—2017年半干旱牧区天然打草场实际生产力与潜在生产力均随降水增加呈上升趋势,天然打草场18年平均实际生产力和潜在生产力分别为295.24和557.79 g C·m^-2·a^-1。按不同草地类型分析,气候生产潜力与实际生产潜力均以草甸草原最高,分别为589.68 g C·m^-2·a^-1和349.78 g C·m^-2·a^-1,山地草甸的气候生产潜力最低,为518.72 g C·m^-2·a^-1,而实际生产潜力以典型草原最低,仅为269.52 g C·m^-2·a^-1。从变异系数来分析,气候生产潜力与实际生产力均以草甸草原最稳定。从年际变化率分析,草甸草原的气候生产潜力的上升速率最高,为6.30 g C·m^-2·a^-1,实际生产力以山地草甸上升速率最高,为4.44 g C·m^-2·a^-1。实际生产力对降水的响应高于温度,其中95.88%的打草场与降水呈显著正相关关系,与温度呈负相关的区域仅占总面积的5.70%,且不同草地类型的实际生产力均与降水在P<0.001水平呈显著正相关关系。【结论】天然打草场气候生产潜力呈由西向东递增的地带性规律,而实际生产力受水热条件的影响,以大兴安岭为中心向东西两麓逐渐递减,其对降水的响应高于温度,水分条件是该区植被生长的限制因子;年均气候资源利用率的分布规律与实际生产力相同,平均气候资源利用率为55.09%;以草甸草原打草场的气候资源利用率最高,高达60.34%,同时也是退化速度最高的草地类型。展开更多
Climate warming is expected to influence forest growth,composition and distribution.However,accurately estimating and predicting forest biomass,potential productivity or forest growth is still a challenge for forest m...Climate warming is expected to influence forest growth,composition and distribution.However,accurately estimating and predicting forest biomass,potential productivity or forest growth is still a challenge for forest managers dealing with land-use at the stand to regional levels.In the present study,we predicted the potential productivity(PP)of forest under current and future climate scenarios(RCP2.6,RCP4.5,RCP6.0 and RCP8.5)in Jilin province,northeastern China by using Paterson’s Climate Vegetation and Productivity(CVP)index model.The PP was validated by comparing it with the mean and maximum net primary production calculated from light energy utilization(GLM_PEM).Our results indicated that using the CVP index model is partially valid for predicting the potential forest productivity in northeastern China.PP exhibited obvious spatial heterogeneity varying from 4.6 to 8.9 m3 ha-1 year-1 with an increasing tendency from northwest to southeast driven by the precipitation across the region.The number of vegetation-active months,precipitation and insolation coefficient were identified as the primary factors affecting PP,but no significant relationship was found for warmest temperature or temperature fluctuation.Under future climate scenarios,PP across the Jilin Province is expected to increase from 1.38%(RCP2.6 in 2050)to 15.30%(RCP8.5 in 2070),especially in the eastern Songnen Plain(SE)for the RCP8.5 scenarios.展开更多
The impact of climate change on maize potential productivity and the potential productivity gap in Southwest China（SWC） are investigated in this paper.We analyze the impact of climate change on the photosynthetic,li...The impact of climate change on maize potential productivity and the potential productivity gap in Southwest China（SWC） are investigated in this paper.We analyze the impact of climate change on the photosynthetic,light-temperature,and climatic potential productivity of maize and their gaps in SWC,by using a crop growth dynamics statistical method.During the maize growing season from 1961 to 2010,minimum temperature increased by 0.20℃ per decade（p 〈 0.01） across SWC.The largest increases in average and minimum temperatures were observed mostly in areas of Yunnan Province.Growing season average sunshine hours decreased by 0.2 h day^（-1） per decade（p 〈 0.01） and total precipitation showed an insignificant decreasing trend across SWC.Photosynthetic potential productivity decreased by 298 kg ha^（-1）per decade（p 〈 0.05）.Both light-temperature and climatic potential productivity decreased（p 〈 0.05） in the northeast of SWC,whereas they increased（p 〈 0.05） in the southwest of SWC.The gap between lighttemperature and climatic potential productivity varied from 12 to 2729 kg ha^（-1）,with the high value areas centered in northern and southwestern SWC.Climatic productivity of these areas reached only 10%-24%of the light-temperature potential productivity,suggesting that there is great potential to increase the maize potential yield by improving water management in these areas.In particular,the gap has become larger in the most recent 10 years.Sensitivity analysis shows that the climatic potential productivity of maize is most sensitive to changes in temperature in SWC.The findings of this study are helpful for quantification of irrigation water requirements so as to achieve maximum yield potentials in SWC.展开更多
基金Key Project of National Natural Science Foundation of China,No.41530749 Science and Technology Project of Sichuan Provincial Department of Education,No.15ZB0023+1 种基金 Youth Projects of National Natural Science Foundation of China,No.41301196,No.41501202 Chongqing Foundation and Advanced Research Project,No.cstc2014jcyj A0808
文摘Using the Integrated Biosphere Simulator, a dynamic vegetation model, this study initially simulated the net primary productivity（NPP） dynamics of China＇s potential vegetation in the past 55 years（1961–2015） and in the future 35 years（2016–2050）. Then, taking the NPP of the potential vegetation in average climate conditions during 1986–2005 as the basis for evaluation, this study examined whether the potential vegetation adapts to climate change or not. Meanwhile, the degree of inadaptability was evaluated. Finally, the NPP vulnerability of the potential vegetation was evaluated by synthesizing the frequency and degrees of inadaptability to climate change. In the past 55 years, the NPP of desert ecosystems in the south of the Tianshan Mountains and grassland ecosystems in the north of China and in western Tibetan Plateau was prone to the effect of climate change. The NPP of most forest ecosystems was not prone to the influence of climate change. The low NPP vulnerability to climate change of the evergreen broad-leaved and coniferous forests was observed. Furthermore, the NPP of the desert ecosystems in the north of the Tianshan Mountains and grassland ecosystems in the central and eastern Tibetan Plateau also had low vulnerability to climate change. In the next 35 years, the NPP vulnerability to climate change would reduce the forest–steppe in the Songliao Plain, the deciduous broad-leaved forests in the warm temperate zone, and the alpine steppe in the central and western Tibetan Plateau. The NPP vulnerability would significantly increase of the temperate desert in the Junggar Basin and the alpine desert in the Kunlun Mountains. The NPP vulnerability of the subtropical evergreen broad-leaved forests would also increase. The area of the regions with increased vulnerability would account for 27.5% of China.
文摘【目的】定量评估半干旱牧区天然打草场的生产能力,分析天然打草场的退化程度,明确气候因子对打草场生长过程的影响。【方法】利用Miami和Tharnthwaite Memorial模型计算2000—2017年半干旱牧区天然打草场气候生产潜力,并结合近18年的中分辨率成像光谱仪(MODIS)净初级生产力(NPP)产品(MOD17A2H)进行分析。【结果】2000—2017年半干旱牧区天然打草场实际生产力与潜在生产力均随降水增加呈上升趋势,天然打草场18年平均实际生产力和潜在生产力分别为295.24和557.79 g C·m^-2·a^-1。按不同草地类型分析,气候生产潜力与实际生产潜力均以草甸草原最高,分别为589.68 g C·m^-2·a^-1和349.78 g C·m^-2·a^-1,山地草甸的气候生产潜力最低,为518.72 g C·m^-2·a^-1,而实际生产潜力以典型草原最低,仅为269.52 g C·m^-2·a^-1。从变异系数来分析,气候生产潜力与实际生产力均以草甸草原最稳定。从年际变化率分析,草甸草原的气候生产潜力的上升速率最高,为6.30 g C·m^-2·a^-1,实际生产力以山地草甸上升速率最高,为4.44 g C·m^-2·a^-1。实际生产力对降水的响应高于温度,其中95.88%的打草场与降水呈显著正相关关系,与温度呈负相关的区域仅占总面积的5.70%,且不同草地类型的实际生产力均与降水在P<0.001水平呈显著正相关关系。【结论】天然打草场气候生产潜力呈由西向东递增的地带性规律,而实际生产力受水热条件的影响,以大兴安岭为中心向东西两麓逐渐递减,其对降水的响应高于温度,水分条件是该区植被生长的限制因子;年均气候资源利用率的分布规律与实际生产力相同,平均气候资源利用率为55.09%;以草甸草原打草场的气候资源利用率最高,高达60.34%,同时也是退化速度最高的草地类型。
文摘Climate warming is expected to influence forest growth,composition and distribution.However,accurately estimating and predicting forest biomass,potential productivity or forest growth is still a challenge for forest managers dealing with land-use at the stand to regional levels.In the present study,we predicted the potential productivity(PP)of forest under current and future climate scenarios(RCP2.6,RCP4.5,RCP6.0 and RCP8.5)in Jilin province,northeastern China by using Paterson’s Climate Vegetation and Productivity(CVP)index model.The PP was validated by comparing it with the mean and maximum net primary production calculated from light energy utilization(GLM_PEM).Our results indicated that using the CVP index model is partially valid for predicting the potential forest productivity in northeastern China.PP exhibited obvious spatial heterogeneity varying from 4.6 to 8.9 m3 ha-1 year-1 with an increasing tendency from northwest to southeast driven by the precipitation across the region.The number of vegetation-active months,precipitation and insolation coefficient were identified as the primary factors affecting PP,but no significant relationship was found for warmest temperature or temperature fluctuation.Under future climate scenarios,PP across the Jilin Province is expected to increase from 1.38%(RCP2.6 in 2050)to 15.30%(RCP8.5 in 2070),especially in the eastern Songnen Plain(SE)for the RCP8.5 scenarios.
基金Supported by the National Basic Research and Development (973) Program of China(2013CB430205)
文摘The impact of climate change on maize potential productivity and the potential productivity gap in Southwest China（SWC） are investigated in this paper.We analyze the impact of climate change on the photosynthetic,light-temperature,and climatic potential productivity of maize and their gaps in SWC,by using a crop growth dynamics statistical method.During the maize growing season from 1961 to 2010,minimum temperature increased by 0.20℃ per decade（p 〈 0.01） across SWC.The largest increases in average and minimum temperatures were observed mostly in areas of Yunnan Province.Growing season average sunshine hours decreased by 0.2 h day^（-1） per decade（p 〈 0.01） and total precipitation showed an insignificant decreasing trend across SWC.Photosynthetic potential productivity decreased by 298 kg ha^（-1）per decade（p 〈 0.05）.Both light-temperature and climatic potential productivity decreased（p 〈 0.05） in the northeast of SWC,whereas they increased（p 〈 0.05） in the southwest of SWC.The gap between lighttemperature and climatic potential productivity varied from 12 to 2729 kg ha^（-1）,with the high value areas centered in northern and southwestern SWC.Climatic productivity of these areas reached only 10%-24%of the light-temperature potential productivity,suggesting that there is great potential to increase the maize potential yield by improving water management in these areas.In particular,the gap has become larger in the most recent 10 years.Sensitivity analysis shows that the climatic potential productivity of maize is most sensitive to changes in temperature in SWC.The findings of this study are helpful for quantification of irrigation water requirements so as to achieve maximum yield potentials in SWC.
