Kuzyk, Z A; Macdonald, R W; Granskog, Mats A; Scharien, R K; Galley, R J; Michel, Christine; Barber, D; Stern, G (2008): Water chemistry and heat budget of the Churchill River estuary region. PANGAEA, https://doi.org/10.1594/PANGAEA.813410, Supplement to: Kuzyk, ZA et al. (2008): Sea ice, hydrological, and biological processes in the Churchill River estuary region, Hudson Bay. Estuarine, Coastal and Shelf Science, 77(3), 369-384, https://doi.org/10.1016/j.ecss.2007.09.030
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A conceptual scheme for the transition from winter to spring is developed for a small Arctic estuary (Churchill River, Hudson Bay) using hydrological, meteorological and oceanographic data together with models of the landfast ice. Observations within the Churchill River estuary and away from the direct influence of the river plume (Button Bay), between March and May 2005, show that both sea ice (production and melt) and river water influence the region's freshwater budget. In Button Bay, ice production in the flaw lead or polynya of NW Hudson Bay result in salinization through winter until the end of March, followed by a gradual freshening of the water column through April-May. In the Churchill Estuary, conditions varied abruptly throughout winter-spring depending on the physical interaction among river discharge, the seasonal landfast ice, and the rubble zone along the seaward margin of the landfast ice. Until late May, the rubble zone partially impounded river discharge, influencing the surface salinity, stratification, flushing time, and distribution and abundance of nutrients in the estuary. The river discharge, in turn, advanced and enhanced sea ice ablation in the estuary by delivering sensible heat. Weak stratification, the supply of riverine nitrogen and silicate, and a relatively long flushing time (~6 days) in the period preceding melt may have briefly favoured phytoplankton production in the estuary when conditions were still poor in the surrounding coastal environment. However, in late May, the peak flow and breakdown of the ice-rubble zone around the estuary brought abrupt changes, including increased stratification and turbidity, reduced marine and freshwater nutrient supply, a shorter flushing time, and the release of the freshwater pool into the interior ocean. These conditions suppressed phytoplankton productivity while enhancing the inventory of particulate organic matter delivered by the river. The physical and biological changes observed in this study highlight the variability and instability of small frozen estuaries during winter-spring transition, which implies sensitivity to climate change.
Median Latitude: 58.900370 * Median Longitude: -93.748860 * South-bound Latitude: 58.673700 * West-bound Longitude: -94.288400 * North-bound Latitude: 59.900000 * East-bound Longitude: -90.000000
Date/Time Start: 2005-03-14T00:00:00 * Date/Time End: 2005-10-14T00:00:00
Datasets listed in this publication series
- Kuzyk, ZA; Macdonald, RW; Granskog, MA et al. (2008): (Table 2) Oxygen isotopic ratios in water samples from Churchill River, Button Bay and Hudson Bay. https://doi.org/10.1594/PANGAEA.813406
- Kuzyk, ZA; Macdonald, RW; Granskog, MA et al. (2008): (Table 3) Equivalent heights of river water and sea ice melt in the Churchill River estuary and Button Bay, and estuary flushing times based on Churchill River discharge. https://doi.org/10.1594/PANGAEA.813407
- Kuzyk, ZA; Macdonald, RW; Granskog, MA et al. (2008): (Table 4) Heat budget elements contributing to sea ice melt in the Churchill River estuary region. https://doi.org/10.1594/PANGAEA.813408
- Kuzyk, ZA; Macdonald, RW; Granskog, MA et al. (2008): (Table 5) Concentrations of dissolved nutrients in Button Bay and the Churchill River estuary region. https://doi.org/10.1594/PANGAEA.813409