Titlebook: Lakes of Mongolia; Geomorphology, Geoch Alexander Orkhonselenge,Munkhjargal Uuganzaya,Tuya Book 2022 The Editor(s) (if applicable) and The

dictator

Lake Khukhing 1989–2015 was moderately related to temperature (. = 0.6705), but it had no clear relationship with precipitation (. = 0.0453). The correlation analysis shows that the lake area between 1989 and 2015 had a strong negative correlation with temperature (. = −0.818) and a weak positive correlation

embolus

假装是你

Lake Ulaanis shows that the lake area during 1986–2014 had a weak positive correlation with air temperature (. = 0.288) but no clear correlation with precipitation (. = 0.07). The geochemical analysis shows the dominance of alkali and alkaline earth metals in Lake Ulaan sediments and the higher degree of chem

prolate

凝视

Lake Uvsvironmental conditions linked to histories of glacial, fluvial, aeolian, lacustrine, and Govi environments in the Depression of Great Lakes and the Mongolian Altai Mountain Range, which are major physiographic components in western Mongolia, Eurasia, and Central Asia.

kyphoplasty

Lake Khotonr temperature (. = 0.0004). The correlation analysis shows that the lake area during 2010–2015 had a weak positive correlation with precipitation (. = 0.289) and a weak negative correlation with air temperature (. = −0.021). Nevertheless, short-term data are still insufficient to infer these relatio

FIN

Landscape, Lake Distribution, and Evolution in Northern Mongoliaave primarily tectonic, glacial, fluvial, and thermokarst origins. Geochemical, geochronological, and hydrological records obtained in northern Mongolia would potentially lead to understanding of the geomorphological and sedimentological processes in the region, and they could help in reconstructing

Obverse

Lake Khuvsgulecipitation (. = 0.1059) recorded at the northern shore of the lake, and here the correlation analysis shows that the lake area had weak negative correlations with both air temperature (. = −0.378) and precipitation (. = −0.325). The lake area during 1970–2015 had weak linear relationships with the

PALL

Lake Khargalcipitation (. = 0.139), but it was not clearly related to the annual average air temperature (. = 0.0187). The correlation analysis shows that the lake area during 1986–2018 had a weak positive correlation with air temperature (. = 0.136) and a weak negative correlation with precipitation (. = −0.37

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