scholarly journals How do persistent organic pollutants be coupled with biogeochemical cycles of carbon and nutrients in terrestrial ecosystems under global climate change?

2012 ◽  
Vol 12 (3) ◽  
pp. 411-419 ◽  
Author(s):  
Ying Teng ◽  
Zhihong Xu ◽  
Yongming Luo ◽  
Frédérique Reverchon
2021 ◽  
Vol 2 (1) ◽  
Author(s):  
Yuhao Feng ◽  
Haojie Su ◽  
Zhiyao Tang ◽  
Shaopeng Wang ◽  
Xia Zhao ◽  
...  

AbstractGlobal climate change likely alters the structure and function of vegetation and the stability of terrestrial ecosystems. It is therefore important to assess the factors controlling ecosystem resilience from local to global scales. Here we assess terrestrial vegetation resilience over the past 35 years using early warning indicators calculated from normalized difference vegetation index data. On a local scale we find that climate change reduced the resilience of ecosystems in 64.5% of the global terrestrial vegetated area. Temperature had a greater influence on vegetation resilience than precipitation, while climate mean state had a greater influence than climate variability. However, there is no evidence for decreased ecological resilience on larger scales. Instead, climate warming increased spatial asynchrony of vegetation which buffered the global-scale impacts on resilience. We suggest that the response of terrestrial ecosystem resilience to global climate change is scale-dependent and influenced by spatial asynchrony on the global scale.


2015 ◽  
Vol 9 (4) ◽  
pp. 201-208 ◽  
Author(s):  
Dubey Garima ◽  
Kollah Bharati ◽  
Ahirwar Usha ◽  
Tiwari Sneh ◽  
Ranjan Mohanty Santosh

2011 ◽  
Vol 6 (4) ◽  
pp. 169-175
Author(s):  
Jonathan P. Zehr ◽  
Julie Robidart ◽  
Chris Scholin

2019 ◽  
Vol 488 (1) ◽  
pp. 74-80
Author(s):  
S. N. Denisov ◽  
A. V. Eliseev ◽  
I. I. Mokhov

Obtained the estimates of the contribution of anthropogenic and natural GHG emissions into the atmosphere from the territory of Russia to global climate change under various scenarios of anthropogenic impact in the 21st century. Accounting for changes in climatic conditions can strongly influence the indicators of the impact of various greenhouse gas emissions on the climate system, especially at large time horizons. Moreover, depending on the planning horizon, the role of the natural fluxes of greenhouse gases into the atmosphere from terrestrial ecosystems may change. Currently, terrestrial ecosystems in the Russian regions affect global temperature in both directions: absorbing CO2 from the atmosphere contributes to slowing its growth, and emitting CH4 into the atmosphere accelerates warming. The net effect of the natural fluxes of these greenhouse gases from the Russian regions in modern conditions helps to slow down warming. This net effect is increasing in the first half of the 21st century, and after reaching a maximum (depending on the anthropogenic emission scenario) decreases by the end of the century under all the considered anthropogenic impact scenarios due to an increase in natural CH4 emissions and a decrease in CO2 absorption by terrestrial ecosystems.


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