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<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>Yong Liu</dc:contributor>
  <dc:contributor>Yaoyang Xu</dc:contributor>
  <dc:contributor>Tyler Wagner</dc:contributor>
  <dc:creator>Zhongyao Liang</dc:creator>
  <dc:date>2021</dc:date>
  <dc:description>Dimethyl sulfide (DMS) serves as an anti-greenhouse gas, plays multiple roles
7   in aquatic ecosystems, and contributes to the global sulfur cycle.  The chlorophyll
8   a (CHL, an indicator of phytoplankton biomass)-DMS relationship is critical for
9   estimating DMS emissions from aquatic ecosystems. Importantly, recent research has
10   identified that the CHL-DMS relationship has a breakpoint, where the relationship
11   is  positive  below  a  CHL  threshold  and  negative  at  higher  CHL  concentrations.
12   Conventionally, mean regression methods are employed to characterize the CHL-DMS
13   relationship.  However, these approaches focus on the response of mean conditions
14   and cannot illustrate responses of other parts of the DMS distribution, which could
15   be important in order to obtain a complete view of the CHL-DMS relationship.  In
16   this study, for the first time, we proposed a novel Bayesian change point quantile
17   regression (BCPQR) model that integrates and inherits advantages of Bayesian change
18   point models and Bayesian quantile regression models. Our objective was to examine
19   whether or not the BCPQR approach could enhance the understanding of shifting
20   CHL-DMS relationships in aquatic ecosystems. We fitted BCPQR models at five
21   regression quantiles for freshwater lakes and for seas. We found that BCPQR models
22   could provide a relatively complete view on the CHL-DMS relationship. In particular,
23   it quantified the upper boundary of the relationship, representing the limiting effect of
24   CHL on DMS. Based on the results of paired parameter comparisons, we revealed the
25   inequality of regression slopes in BCPQR models for seas, indicating that applying
26   the mean regression method to develop the CHL-DMS relationship in seas might not
27   be appropriate. We also confirmed relationship differences between lakes and seas at
28   multiple regression quantiles.  Further, by introducing the concept of DMS emission
29   potential, we found that pH was not likely a key factor leading to the change of the
30   CHL-DMS relationship in lakes.  These findings cannot be revealed using piecewise
31   linear regression. We thereby concluded that the BCPQR model does indeed enhance
 
32   the understanding of shifting CHL-DMS relationships in aquatic ecosystems and is
33   expected to benefit efforts aimed at estimating DMS emissions. Considering  that
34   shifting (threshold) relationships are not rare and that the BCPQR model can easily
35   be adapted to different systems,  the BCPQR approach is expected to have great
36   potential for generalization in other environmental and ecological studies.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/j.watres.2021.117287</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Elsevier</dc:publisher>
  <dc:title>Bayesian change point quantile regression approach to enhance the understanding of shifting phytoplankton-dimethyl sulfide relationships in aquatic ecosystems</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>