| Literature DB >> 26022331 |
Emma Undeman1, Bo G Gustafsson, Christoph Humborg, Michael S McLachlan.
Abstract
Organic contaminants constitute one of many stressors that deteriorate the ecological status of the Baltic Sea. When managing environmental problems in this marine environment, it may be necessary to consider the interactions between various stressors to ensure that averting one problem does not exacerbate another. A novel modeling tool, BALTSEM-POP, is presented here that simulates interactions between climate forcing, hydrodynamic conditions, and water exchange, biogeochemical cycling, and organic contaminant transport and fate in the Baltic Sea. We discuss opportunities to use the model to support different aspects of chemicals management. We exemplify these opportunities with a case study where two emission-reduction strategies for a chemical used in personal care products (decamethylcyclopentasiloxane) are evaluated, and where the confounding influence of future climate change and eutrophication on the impact of the emission-reduction strategies are assessed.Entities:
Mesh:
Year: 2015 PMID: 26022331 PMCID: PMC4447700 DOI: 10.1007/s13280-015-0668-2
Source DB: PubMed Journal: Ambio ISSN: 0044-7447 Impact factor: 5.129
Fig. 1Predicted surface water concentrations (dissolved, in pg L−1 bulk water at 10-m depth) in the Gotland Sea and Bothnian Bay with emissions either constant at current levels, emissions via rivers reduced (year 2006) by 90 %, or air concentrations reduced by 90 % (labeled current, red. river load, and red. air conc. in the legend, respectively). The forcing scenario RWCL was used, i.e., the nutrient loads were fixed at a level representing the average between 1997 and 2003 (constant load, CL), and the climate scenario represents a random weather (RW) similar to today’s conditions (no further global warming)
Fig. 2Predicted surface water concentrations (dissolved, in pg L−1 bulk water at 10-m depth) in the Gotland Sea and Bothnian Bay during two time periods (2019–2022 and 2097–2100) calculated using five different scenarios for climate change and nutrient loads. See also Fig. S5 in the Supplementary material