supported by the National Natural Science Foundation of China(Nos.42371150,U2268216);the State Key Laboratory of Frozen Soil Engineering(No.SKLFSEZT-202116);the Youth Innovation Promotion Association of the Chinese Academy of Sciences(Nos.2023445,2020421);the CAS Western Young Scholars Project to Dongliang Luo。
0 INTRODUCTION The Sixth Assessment Report of the Intergovernmental Panel on Climate Change(IPCC AR6)indicated that the global surface temperature had risen by approximately 1.09℃compared to the 1850-1900 average ove...
supported by the National Natural Science Foundation of China(32241034,32425004,42141006);the CAS Project for Young Scientists in Basic Research(YSBR-037);the National Key Research and Development Program of China(2022YFF0801903);the New Cornerstone Science Foundation through the XPLORER PRIZE;supported by the Spanish Government grants PID2022-140808NB-I00 and TED2021-132627 B-I00 funded by MCIN,AEI/10.13039/501100011033 European Union Next Generation EU/PRTR。
Our knowledge on permafrost carbon(C)cycle is crucial for understanding its feedback to climate warming and developing nature-based solutions for mitigating climate change.To understand the characteristics of permafro...
supported by the National Natural Science Foundation of China(Grants No.42201015,U2240217,and U2340213);the Jiangsu Funding Program for Excellent Postdoctoral Talent(Grant No.2022ZB173);the Special Fund of the National Key Laboratory of Water Disaster Prevention(Grant No.523024862).
The Tibetan Plateau(TP)has undergone significant warming and humidification in recent years,resulting in rapid permafrost degradation and spatiotemporal variations in hydrological processes,such as subsurface water tr...
We acknowledged the main support from the Second Tibetan Plateau Scientific Expedition and Research(STEP)program(2019QZKK0905);the National Science Foundation of China(42371150,U2268216);the Youth Science and Technology Talent Lifting Project of Gansu Province(GXH20220530-08);the State Key Laboratory of Frozen Soil Engineering(SKLFSE-ZT-202116);the Youth Innovation Promotion Association of the Chinese Academy of Sciences(2023445,2020421).
Thermokarst lake formation accelerates permafrost degradation due to climate warming,thereby releasing significant amounts of carbon into the atmosphere,complicating hydrological cycles,and causing environmental damag...
supported by the National Science Fund for Distinguished Young Scholars[41925027].
Climate warming rates in the Arctic are far greater than the global average,exerting stronger impacts on permafrost degradation and thermokarst landform development.Thermokarst lakes and ponds(TLPs),which are widely d...
funded by the National Natural Science Foundation of China(42372334);the Science and Technology Research and Development Program of the Qinghai-Tibet Group Corporation(Grant No.QZ2022-G05)。
Under the rapidly warming climate in the Arctic and high mountain areas,permafrost is thawing,leading to various hazards at a global scale.One common permafrost hazard termed retrogressive thaw slump(RTS)occurs extens...
supported by the Natural Science Foundation of Qinghai Province,China(No.2021-ZJ940Q);the Open Project of State Key Laboratory of Plateau Ecology and Agriculture,Qinghai University(No.2022-ZZ-02)。
As significant evidence of permafrost degradation,thermokarst lakes play an important role in the permafrost regions by regulating hydrology,ecology,and biogeochemistry.In the Sources Area of the Yellow River(SAYR),pe...
supported by Independent Research Project of State Key Laboratory of Frozen Soil Engineering(SKLFSE-ZQ-50);CAS Youth talent growth fund(Y9510608);National Key R&D(2017YFC0405101);National Natural Science Foundation of China(41901079).
In permafrost regions of the Qinghai-Tibet Plateau,road disaster caused by permafrost degradation cannot be ignored.As a common thermal disaster in permafrost regions,thermokarst lake has serious thermal erosion on pe...
This study presents thermokarst lake changes at seven different sites in the continuous and isolated permafrost zones in Mongolia. Lakes larger than 0.1 ha were analyzed using Corona KH-4, KH-4A and KH-4B (1962-1968),...
supported by the National Basic Research Program of China (2012CB026101);the Western Project Program of the Chinese Academy of Sciences (KZCX2-XB3-19);the National Sci-Tech Support Plan (2014BAG05B01)
This work presents changes of thermokarst lakes from Beilu River Basin on the Qinghai-Tibet Plateau over the past four decades (1969-2010) using aerial and satellite image interpretation. The results indicated that ...