Physical and chemical limnology of a subsaline athalassic lake in West Greenland

• Main Authors: Willemse, Nicolaas W., Van Dam, Oscar, Van Helvoort, Pieter Jan, Dankers, Rutger, Brommer, Marit, Schokker, Jeroen, Valstar, Tessa E., De Wolf, Hein
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2004
• Subjects: Greenland; arctic; hydrology; limnology; meromixis; meteorological data; saline lakes; Arctic; Basin Lake; greenlandic; Phytoplankton
• Online Access: https://research.wur.nl/en/publications/physical-and-chemical-limnology-of-a-subsaline-athalassic-lake-in; https://doi.org/10.1023/B:HYDR.0000036132.96154.01

Physical and chemical profiles of a shallow (c. 12-m-deep) subsaline (total dissolved solids 2.3-2.8 g l -1) closed-basin lake in the continental area of southwestern Greenland are described for the first time. Watercolumn data for every 5th consecutive day between April 20 and October 6, 2001, and continuous recordings of lake water level and meteorological conditions are used to infer controls on contemporary lake functioning, sediment formation and climate-lake interactions. Limnological observations demonstrate the importance of lake-ice formation and its role in haline convection and the development of meromixis. Observed lake cycling suggest that the lake at present is in a state of near-meromixis where stagnant bottom waters de-stratify through deep penetration of weak haline convective cells by the end of June. From this study, the primary reasons the shallow Greenlandic low salinity lakes develop meromixis are: (i) lack of an outflow (ii) meltwater dilution and chemical stratification of surface waters, (iii) insubstantial wind mixing, (iv) a weak winter thermohaline convective cell forced by cryoconcentration, and (v) biogeochemically enhanced solute concentrations near the sediment bed. Throughout the open water period the hydrological balance is dominated by evaporative losses. Lake surface water conductivities change from 2110 to 2890 μS cm -1 due to the combined effects of open water evaporation, meltwater dilution, diffusive exchanges over the seasonal pycnocline, and boundary mixing. Freeze-out of salts and resulting deep haline convection increase overall water column salinity during winter. Owing to deep convective mixing, plant nutrients are relatively high in the upper watercolumn with a dominant internal source of phosphorous. Extreme productivity pulses of phytoplankton are observed as soon as sub-ice radiation levels increase and directly after ice-out when sufficient wind mixing can support an intense monospecific diatom bloom of Diatoma spp. leading to the rapid depletion of dissolved ...