Short Title: Recent Morphodynamics of Alpine Lakes in Southern Carpathians Recent Morphodynamics of Alpine Lakes in Southern Carpathian Mountains using High-Resolution Optical Imagery Marius Necsoiu 1 , Marcel Mîndrescu 2 , Alexandru Onaca 3 , Sarah Wigginton 1 1 Southwest Research Institute ® , Geosciences and Engineering Division, 6220 Culebra Road, San Antonio, Texas, United States 2 University of Suceava, Universităţii 13, RO 720229, Suceava, Romania 3 West University of Timișoara, Department of Geography, Str. V. Pârvan 4, Timișoara , Romania E-mail: mnecsoiu@swri.org Abstract This study reveals for the first time the surface area evolution of glacial lakes in the Romanian Carpathians over 47 years. The research also advances our understanding in the potential of satellite-based remote sensing techniques to monitor geomorphologic evolution of 27 rock basins turned into glacial lakes in the Retezat Mountains, Southern Romanian Carpathians. These mountains host most of the glacial lakes in Romania, including both the widest and deepest glacial lakes. Using high-precision orthorectification and co-registration techniques, the surface area extension and reduction of 27 shallow water bodies ranging in size from 0.10 to 9.14 ha was analyzed over two time intervals (1968–2007 and 2007–2014). The total surface area increased only by 1% between 1968 and 2014, with over half of the growth occurring during the last 7 years of the study period. Analysis of the surface area extension and reduction revealed that catchment aspect, catchment size, lake elevation, landcover, topography, and lake depth are the main environmental factors controlling the present state of the glacial lakes in the central part of the Retezat Mountains. The results suggest that the different behavior of glacial lakes within the north-facing valleys compared with the evolution of the lakes settled in southern exposed valleys is mainly due to climatic and geomorphologic particularities of the opposing slopes. On the northern side the lakes are slowly decreasing due to more intense geomorphologic activity of both the erosivity of precipitations and periglacial processes (e.g., gelifraction, mass wasting, and permafrost degradation). High altitude lakes generally are increasing because of the longer duration of the ice cover and the smaller amounts of sediment yielded © 2015. This manuscript version is made available under the Elsevier user license http://www.elsevier.com/open-access/userlicense/1.0/