Estimation of Continental-Basin-Scale Sublimation in the Lena River Basin, Siberia

<table class="table-group" id="tab5"><tr><td><table class="table"><tr><td class="thead-hr" colspan="4"><hr/></td></tr><tr class="thead"><td align="left">Year</td><td align="center">Snowfall (mm)</td><td align="center">Sublimation (mm)</td><td align="center">Ratio of sublimation loss to snowfall (%)</td></tr><tr><td class="thead-hr" colspan="4"><hr/></td></tr><tr><td align="left">CTL9899</td><td align="center">179</td><td align="center">29</td><td align="center">16.2</td></tr><tr><td align="left">CTL9900</td><td align="center">162</td><td align="center">24</td><td align="center">14.8</td></tr><tr class="table-tr"><td colspan="4"><hr class="tbody-hr"/></td></tr></table></td></tr></table>

Winter water balance and meteorological components in the basin in CTL9899 and CTL9900.

Advances in Meteorology

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Table 5

Table 5: Estimation of Continental-Basin-Scale Sublimation in the Lena River Basin, Siberia 