The spatial and spectral heterogeneity of urban areas makes land cover classification a
challenging process. In this study, we highlight the potential of combined multi-spectral Sentinel-…

Permafrost in Mongolia is located in the transition zone between high-latitude and high-altitude
permafrost regions of the Northern Hemisphere, with large temperature differences and …

Vegetation dynamics in Qinghai-Tibet Plateau (QTP) have been debated in recent decades.
Most studies suggest that wetter and warmer climatic conditions would release low …

Large stocks of soil organic carbon (SOC) accumulated in the Northern Hemisphere permafrost
regions may be vulnerable to climatic warming, but global estimates of SOC distribution …

Soil organic carbon (SOC) is very important in the vulnerable ecological environment of the
Third Pole; however, data regarding the spatial distribution of SOC are still scarce and …

During the past several decades, desertification and land degradation have become more
and more serious in Mongolia. The drivers of land use/cover change (LUCC), such as …

The thawing of permafrost on the Qinghai-Tibet Plateau (QTP) leads to more frequent occurrences
of thaw slump (TS), which have significant impacts on local ecosystems, carbon cycles…

Local climate zone (LCZ) maps have been used widely to study urban structures and urban
heat islands. Because remote sensing data enable automated LCZ mapping on a large scale…

Permafrost degradation on the Qinghai—Tibet Plateau (QTP) directly affects evapotranspiration
and moisture recycling processes by changing the underlying land surface conditions. …

Mongolia's ecosystem is highly vulnerable to both climate change and overgrazing, which
threaten its ecological stability and livestock husbandry. However, insufficient high-quality …