Permafrost thaw and thermokarst in the source region of the Yangtze river in the central Tibetan plateau revealed by radar and optical remote sensing.

MLA

Wang, Lingxiao, et al. “Permafrost Thaw and Thermokarst in the Source Region of the Yangtze River in the Central Tibetan Plateau Revealed by Radar and Optical Remote Sensing.” Earth Surface Processes & Landforms, vol. 49, no. 13, Oct. 2024, pp. 4324–39. EBSCOhost, https://doi.org/10.1002/esp.5969.

APA

Wang, L., Huang, C., Zhao, L., Zhou, H., Liu, S., Tang, Y., Li, Z., Xiao, Y., Zou, D., Liu, G., Du, E., Hu, G., & Wang, C. (2024). Permafrost thaw and thermokarst in the source region of the Yangtze river in the central Tibetan plateau revealed by radar and optical remote sensing. Earth Surface Processes & Landforms, 49(13), 4324–4339. https://doi.org/10.1002/esp.5969

Chicago

Wang, Lingxiao, Chenqi Huang, Lin Zhao, Huayun Zhou, Shibo Liu, Yunqi Tang, Zhibin Li, et al. 2024. “Permafrost Thaw and Thermokarst in the Source Region of the Yangtze River in the Central Tibetan Plateau Revealed by Radar and Optical Remote Sensing.” Earth Surface Processes & Landforms 49 (13): 4324–39. doi:10.1002/esp.5969.