Abstract:Abstract. The paper reviews critical processes for the landsea fluxes of biogenic elements (C, N, P, Si) in the Baltic Sea catchment and discusses possible future scenarios as a consequence of improved sewage treatment, agricultural practices and increased hydropower demand (for N, P and Si) and of global warming, i.e., changes in hydrological patterns (for C). These most significant drivers will not only change the total amount of nutrient inputs and fluxes of organic and inorganic forms of carbon to the Balt… Show more
“…DSi yields are also generally low in Arctic rivers (Dittmar & Kattner, ), with average DSi flux of the six largest rivers draining into the Arctic ranging from 32 to 82 mol DSi day −1 km −2 (average 54.4) (Holmes et al, ). The DSi concentrations and yields observed (Table ) from the most northern rivers in our study fall within that range expected of Arctic rivers, while the more southern rivers in this study display values typical of rivers draining boreal landscapes (Dürr et al, ; Humborg et al, ; Phillips & Cowling, ). The majority of DSi was exported during the freshet or summer period, while the least amount was exported during the winter, a seasonal pattern typical of high latitude rivers (Guo et al, ; Holmes et al, ).…”
Silicon (Si) exports from terrestrial to marine systems can dictate phytoplankton species composition in Arctic coastal waters. Diatoms are often the dominant autotroph in Arctic waters, making Si an important control on Arctic marine primary productivity. Yet even as Arctic regions are among the fastest warming on Earth, we lack baseline knowledge on the magnitudes and controls of Arctic river Si exports. To address uncertainties in current and future Si behavior, we used a combination of field data and modeling to quantify daily yields of dissolved Si (DSi) and biogenic Si (BSi) from a 400 km space‐for‐time latitudinal gradient of seven basins across the boreal‐Arctic transition in Alaska (United States) over the course of 2 years (2015–2016). Mean annual DSi concentrations (33–149 μM) and yields (13–49 kmol km−2 year−1) were significantly and positively correlated with mean basin active layer depth, indicating that permafrost thaw will likely increase DSi fluxes to Arctic coastal waters. Conversely, BSi concentrations (7–16 μM) and yields (2.6–4.5 kmol km−2 year−1) were more uniform across the seven basins, indicating that warming may not substantially alter BSi loads to coastal systems in the near future. Our data also indicate that climatic warming will advance the timing of Si delivery to coastal waters in the spring, although the ratios of Si to nitrogen in Arctic river exports will likely remain steady. These results highlight the important role of basin hydrology, largely driven by permafrost extent, as a key driver of Si exchange at the land‐sea interface in the Arctic.
“…DSi yields are also generally low in Arctic rivers (Dittmar & Kattner, ), with average DSi flux of the six largest rivers draining into the Arctic ranging from 32 to 82 mol DSi day −1 km −2 (average 54.4) (Holmes et al, ). The DSi concentrations and yields observed (Table ) from the most northern rivers in our study fall within that range expected of Arctic rivers, while the more southern rivers in this study display values typical of rivers draining boreal landscapes (Dürr et al, ; Humborg et al, ; Phillips & Cowling, ). The majority of DSi was exported during the freshet or summer period, while the least amount was exported during the winter, a seasonal pattern typical of high latitude rivers (Guo et al, ; Holmes et al, ).…”
Silicon (Si) exports from terrestrial to marine systems can dictate phytoplankton species composition in Arctic coastal waters. Diatoms are often the dominant autotroph in Arctic waters, making Si an important control on Arctic marine primary productivity. Yet even as Arctic regions are among the fastest warming on Earth, we lack baseline knowledge on the magnitudes and controls of Arctic river Si exports. To address uncertainties in current and future Si behavior, we used a combination of field data and modeling to quantify daily yields of dissolved Si (DSi) and biogenic Si (BSi) from a 400 km space‐for‐time latitudinal gradient of seven basins across the boreal‐Arctic transition in Alaska (United States) over the course of 2 years (2015–2016). Mean annual DSi concentrations (33–149 μM) and yields (13–49 kmol km−2 year−1) were significantly and positively correlated with mean basin active layer depth, indicating that permafrost thaw will likely increase DSi fluxes to Arctic coastal waters. Conversely, BSi concentrations (7–16 μM) and yields (2.6–4.5 kmol km−2 year−1) were more uniform across the seven basins, indicating that warming may not substantially alter BSi loads to coastal systems in the near future. Our data also indicate that climatic warming will advance the timing of Si delivery to coastal waters in the spring, although the ratios of Si to nitrogen in Arctic river exports will likely remain steady. These results highlight the important role of basin hydrology, largely driven by permafrost extent, as a key driver of Si exchange at the land‐sea interface in the Arctic.
“…P fluxes will decrease due to improved WWT, which is a very likely process as Poland has to follow up the UWWTD. The same tendency of increasing N and decreasing P fluxes was also found by HUMBORG et al (2007). Among the wildcards (extreme scenarios), the adjustment of nutrient surpluses in Poland to the level of Mecklenburg-Western Pomerania would cause the strongest increase in N emissions.…”
Section: Changes In Nutrient Surpluses and Emissions Due To The Scenasupporting
confidence: 61%
“…3) The largest potential for reductions of nutrients from point sources is by im proving waste water treatment (WWT) in the southern and eastern parts of the Baltic Sea catchment (ERIKS- SON et al, 2007;HUMBORG et al, 2007;SCHERNEWSKI et al, 2008).…”
Eutrophication management is still one of the major challenges in the Baltic Sea region. Intense transformation processes in several Baltic Sea states have led to drastic changes in e.g., landuse and thereby nutrient emissions and water quality. Several future development directions are possible. The Oder catchment -lagoon -coastal water system serves as a pilot study area, since it has a major influence on the nutrient loads into the Baltic Sea and about 90% of the catchment is located in Poland, a state with transitional economy. Different scenarios for landuse changes in the Oder catchment are developed and their consequences on nutrient emissions simulated. Next to politically induced changes of agricultural landuse in general, specific aspects such as cultivation of energy maize and increased animal stocks are considered. Nitrogen emissions are likely to increase due to agricultural landuse changes whereas phosphorus emissions will not change or even decrease according to the application of the EC-Urban Waste Water Treatment Directive. Resulting nitrogen loads to the Oder Lagoon could increase up to 23%, phosphorus loads could decrease by 11% compared to 2005. These trends may lead to higher nitrogen availability compared to phosphorus at least in the Oder lagoon. Interannual differences in discharge also have profound effects on nutrient emissions. A good status of the Oder river basin -lagoon -coastal sea system according to EC-Directives is not very likely to be achieved under the investigated circumstances.
“…The decrease will be more pronounced when the efficiency of wastewater treatment is higher by introducing high-grade (tertiary) treatment. This measure together with the increased number of people who are connected to wastewater treatment plants will provide an almost immediate response (Humborg et al 2007;Bryhn 2009 Recently the ministers of the environment of the member states of HELCOM adopted an action plan to considerably reduce the anthropogenic nutrient load to the Baltic Sea and restore a good ecological status by 2021 doi: 10.2166/nh.2012.136 (HELCOM 2007a). To achieve this, country-specific annual nutrient input reduction targets were proposed, based on the principle of maximum allowable nutrient inputs to the sea that were set at the level of about 21,000 tons of phosphorus and 600,000 tons of nitrogen.…”
This study aimed to develop scenarios for a furtiier decrease of point source nutrient load in Estonia to achieve the nutrient réduction target levéis set up by the HELCOM Baltic Sea Action Plan produced' in 2007. A possible reduction in the total phosphorus (TP) and total nitrogen (TN) load has been assessed based on the requirements set up by Estonian and EU legislation as well as the HELCOM recommendations. Scenarios were developed for four urban pollution load classes with different requirements for waste water quality at the outlet of the wastewater treatment plant (WWTP). The results revealed that the load of TP and TN to the sea and to inland surface water bodies can be reduced by 68 and 352 tonnes, respectively, when following the most stringent HELCOM recommendation for the quality of sewerage outlets. These possibly reduced loads form only about 30% of required TP and 40% of TN annual reduction levels in Estonia which are 220 tons of phosphorus and 900 tons of nitrogen. Therefore, further decrease can mostly be made possible by lowering the diffuse load and that can also be problematic.
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