Abstract:A total pollutant load control system (TPLCS) was implemented in the Seto Inland Sea in 1979 to reduce the water pollution and the frequency of red tides. We estimated primary production from 1981 to 2010 to determine the effects of reducing the nutrient loadings from the surrounding land. While primary production has decreased overall in the Seto Inland Sea in response to the TPLCS and the associated reductions in the total nitrogen (T-N) and phosphorus (T-P) loads from land since 1981, the reductions were li… Show more
“…Previous studies have reported that nutrient loadings in Japan have decreased over recent decades (e.g., Yamamoto-Kawai et al 2015;Kamohara et al 2018;Nakai et al 2018), with variable effects on summer pHinsitu in coastal waters. TN was monitored for a shorter period than pHinsitu (1995 to 2009).…”
Section: Regional Differences In Phinsitu Trendsmentioning
confidence: 98%
“…8). The pH trends in coastal areas of western Kyushu, where the anthropogenic nutrient loadings are relatively low, therefore reflect the decreases in nutrient discharges, resulting in variations between regions (e.g., Nakai et al 2018;Yamamoto and Hanazato 2015;Tsuchiya et al, 2018). Several cities in this area have introduced advanced sewage treatment to prevent eutrophication in coastal waters (Nakai et al 2018;Yamamoto and Hanazato 2015).…”
Section: Regional Differences In Phinsitu Trendsmentioning
<p><strong>Abstract.</strong> In recent decades, acidification of the open ocean has shown consistent increases. However, analysis of long-term data in coastal waters shows that the pH is highly variable because of coastal processes and anthropogenic carbon inputs. It is therefore important to understand how anthropogenic carbon inputs and other natural or anthropogenic factors influence the temporal trends in pH in coastal waters. Using water quality data collected at 1481 monitoring sites as part of the Water Pollution Control Program, we determined the long-term trends in pH in Japanese coastal waters at ambient temperature from 1978 to 2009. We found that pH decreased (i.e., acidification) at between 70&#8201;% and 75&#8201;% of the sites and increased (i.e., basification) at between 25&#8201;% and 30&#8201;% of the sites. The rate of decrease varied seasonally and was, on average, &#8722;0.0014&#8201;yr<sup>&#8722;1</sup> in summer and &#8722;0.0024&#8201;yr<sup>&#8722;1</sup> in winter, but with relatively large deviations from these average values. While the overall trends reflect acidification, watershed processes might also have contributed to the large variations in pH in coastal waters. The seasonal variation in the average pH trends reflects variability in warming trends, while regional differences in pH trends are partly related to heterotrophic water processes induced by nutrient loadings.</p>
“…Previous studies have reported that nutrient loadings in Japan have decreased over recent decades (e.g., Yamamoto-Kawai et al 2015;Kamohara et al 2018;Nakai et al 2018), with variable effects on summer pHinsitu in coastal waters. TN was monitored for a shorter period than pHinsitu (1995 to 2009).…”
Section: Regional Differences In Phinsitu Trendsmentioning
confidence: 98%
“…8). The pH trends in coastal areas of western Kyushu, where the anthropogenic nutrient loadings are relatively low, therefore reflect the decreases in nutrient discharges, resulting in variations between regions (e.g., Nakai et al 2018;Yamamoto and Hanazato 2015;Tsuchiya et al, 2018). Several cities in this area have introduced advanced sewage treatment to prevent eutrophication in coastal waters (Nakai et al 2018;Yamamoto and Hanazato 2015).…”
Section: Regional Differences In Phinsitu Trendsmentioning
<p><strong>Abstract.</strong> In recent decades, acidification of the open ocean has shown consistent increases. However, analysis of long-term data in coastal waters shows that the pH is highly variable because of coastal processes and anthropogenic carbon inputs. It is therefore important to understand how anthropogenic carbon inputs and other natural or anthropogenic factors influence the temporal trends in pH in coastal waters. Using water quality data collected at 1481 monitoring sites as part of the Water Pollution Control Program, we determined the long-term trends in pH in Japanese coastal waters at ambient temperature from 1978 to 2009. We found that pH decreased (i.e., acidification) at between 70&#8201;% and 75&#8201;% of the sites and increased (i.e., basification) at between 25&#8201;% and 30&#8201;% of the sites. The rate of decrease varied seasonally and was, on average, &#8722;0.0014&#8201;yr<sup>&#8722;1</sup> in summer and &#8722;0.0024&#8201;yr<sup>&#8722;1</sup> in winter, but with relatively large deviations from these average values. While the overall trends reflect acidification, watershed processes might also have contributed to the large variations in pH in coastal waters. The seasonal variation in the average pH trends reflects variability in warming trends, while regional differences in pH trends are partly related to heterotrophic water processes induced by nutrient loadings.</p>
“…type, magnitude, frequency and timing), connectivity with adjacent systems and differing water quality parameters (Carstensen et al, 2011;Duarte et al, 2015). In successful cases, the improvement appeared in nutrients, Chl.a, dissolved oxygen concentrations and seagrass cover after implementation of the programme (Greening et al, 2014;Riemann et al, 2016;Nakai et al, 2018;Nishijima et al, 2018), whereas little improvement or even worsening were unfortunately reported too (Williams et al, 2010;Riemann et al, 2016).…”
Section: Introductionmentioning
confidence: 99%
“…On the other hand, stable and appropriate primary production by phytoplankton, as well as by seagrasses and benthic microalgae, is essential to sustain the healthy functioning of ecosystems and the sustainable supply of fishery resources (Takai et al, 2002;Hoshika et al, 2006;Nakai et al, 2018). Phytoplankton growth will directly respond to nutrient supply, whereas the growth and distribution of benthic macro-and microalgae will be determined by both nutrient supply and light availability; the latter will also be affected by nutrient supply through phytoplankton growth.…”
Section: Introductionmentioning
confidence: 99%
“…One effect of TPLCS implementation on the Seto Inland Sea has appeared in certain ecosystem components (Yamamoto, 2003;Nakai et al, 2018;Nishijima et al, 2018), although it varies in the subareas. The west-central Seto Inland Sea, including Hiroshima Bay and Aki Nada (Figure 1), receives substantial anthropogenic nutrient loading from its watersheds.…”
Water quality data from 1981 to 2015 were used to elucidate the spatiotemporal distributions of chlorophyll a (Chl.a) concentration and Secchi depth in the west-central Seto Inland Sea, Japan. The results revealed that salinity and distance from the northern coastline were the main factors for predicting Chl.a concentration and Secchi depth, respectively. Significant differences in both of these were observed between subareas in spring, summer and autumn; differences were insignificant in winter. Chl.a concentrations have decreased for the past 35 years, while their extent differed in the subareas. A greater rate of decrease in Chl.a concentration was observed in the innermost Hiroshima Bay in spring, compared with other subareas, while no significant difference in different subareas was found in other seasons. Secchi depth has increased for the past 35 years, but no significant difference in its rate of increase was found among different subareas in all seasons. Total nitrogen loading better explained changes in mean Chl.a concentration than total phosphorus throughout the west-central Seto Inland Sea. Phytoplankton's contributions to light attenuation were low in the west-central Seto Inland Sea, indicating that the nutrient loading reduction programme has been of limited effectiveness in improving water clarity.
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