@misc{hoelemann_seasonal_variability_2005, 
author={Hoelemann, J.A., Schirmacher, M., Prange, A.},
title={Seasonal variability of trace metals in the Lena River and the southeastern Laptev Sea: Impact of the spring freshet},
year={2005},
howpublished = {journal article},
doi = {https://doi.org/10.1016/j.gloplacha.2004.12.008},
abstract = {During the high flow period in June about 35% of the total annual flow of the river Lena flows into the Laptev Sea. Previously published metal budgets for the river Lena that did not incorporate data from the spring high flow period, therefore, underestimate the fluxes of dissolved trace metals from the Siberian rivers to the Arctic Ocean. For instance, the estimated input of dissolved Fe in June 1996 is approximately 4.5 times higher than the average annual dissolved Fe input calculated on the basis of summer data. The results of this study demonstrate that the previous evaluations of the trace metal flux of the Lena river–which are based on data obtained from August to October–may underestimate the total riverine input of dissolved trace metals to the Arctic Ocean.},
note = {Online available at: \url{https://doi.org/10.1016/j.gloplacha.2004.12.008} (DOI). Hoelemann, J.; Schirmacher, M.; Prange, A.: Seasonal variability of trace metals in the Lena River and the southeastern Laptev Sea: Impact of the spring freshet. Global and Planetary Change. 2005. vol. 48, no. 1-3, 112-125. DOI: 10.1016/j.gloplacha.2004.12.008}}