Showing 16,021 - 16,040 results of 227,974 for search '(( 5 ((ppm decrease) OR (mean decrease)) ) OR ( a ((fold decrease) OR (a decrease)) ))', query time: 1.79s Refine Results
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    Panel (a) compares SO<sub>2</sub> emissions prescribed over the historical period in the CMIP5 simulations (solid grey) with three inventory-based estimates of historical emissions... by Nathan P Gillett (557010)

    Published 2013
    “…<p><strong>Figure 1.</strong> Panel (a) compares SO<sub>2</sub> emissions prescribed over the historical period in the CMIP5 simulations (solid grey) with three inventory-based estimates of historical emissions [<a href="http://iopscience.iop.org/1748-9326/8/3/034008/article#erl467068bib1" target="_blank">1</a>, <a href="http://iopscience.iop.org/1748-9326/8/3/034008/article#erl467068bib10" target="_blank">10</a>, <a href="http://iopscience.iop.org/1748-9326/8/3/034008/article#erl467068bib11" target="_blank">11</a>]. …”
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    DataSheet_1_First description of in situ chlorophyll fluorescence signal within East Antarctic coastal polynyas during fall and winter.docx by Lucie Bourreau (16698258)

    Published 2023
    “…An additional signal occurring at 130m depth in August within CDP may result from in situ growth of phytoplankton due to potential adaptation to low irradiance or remnant chlorophyll-a that was advected into the polynya. The decrease and deepening of the fluorescence signal from February to August was accompanied by the deepening of the mixed layer depth and a cooling and salinification of the water column in both polynyas. …”
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    DataSheet_1_First description of in situ chlorophyll fluorescence signal within East Antarctic coastal polynyas during fall and winter.docx by Lucie Bourreau (16698258)

    Published 2023
    “…An additional signal occurring at 130m depth in August within CDP may result from in situ growth of phytoplankton due to potential adaptation to low irradiance or remnant chlorophyll-a that was advected into the polynya. The decrease and deepening of the fluorescence signal from February to August was accompanied by the deepening of the mixed layer depth and a cooling and salinification of the water column in both polynyas. …”
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