40 research outputs found

    Original data in 2018GL077046

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    <p>The original data of the figures in the manuscript of <em>Geophysical Research Letters</em> (2018GL077046) are given in these datasets.</p

    Spatial frequency distribution of anticyclonic and cyclonic eddies annually (a and d), in summer (b and e) and in winter (c and f).

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    Spatial frequency distribution of anticyclonic and cyclonic eddies annually (a and d), in summer (b and e) and in winter (c and f).</p

    The monthly average ΔSST distribution in March, June, September and December.

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    The monthly average ΔSST distribution in March, June, September and December.</p

    Composite of the sea surface height and current surrounding the Mozambique Channel from 2010 to 2019.

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    The study areas are indicated by dashed black squares, i.e., Box N: 10°S–18°S, 40°E–49°E; Box S: 18°S–24°S, 35°E–44°E.</p

    The monthly average climate changes in wind stress (N/m<sup>2</sup>) and EKE (m<sup>2</sup>/s<sup>2</sup>) are represented by dashed lines and solid lines, respectively (a is for Box N and b is for Box S, which are shown in Fig 1).

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    The monthly average climate changes in wind stress (N/m2) and EKE (m2/s2) are represented by dashed lines and solid lines, respectively (a is for Box N and b is for Box S, which are shown in Fig 1).</p

    The seasonal statistics of anticyclonic (a) and cyclonic (b) eddies and ΔSST.

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    The seasonal statistics of anticyclonic (a) and cyclonic (b) eddies and ΔSST.</p

    Origin and developmental trajectories of anticyclonic (a) and cyclonic (b) eddies in the Mozambique Channel.

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    Origin and developmental trajectories of anticyclonic (a) and cyclonic (b) eddies in the Mozambique Channel.</p

    The annual statistics of anticyclonic (a) and cyclonic (b) eddies and ΔSST.

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    The annual statistics of anticyclonic (a) and cyclonic (b) eddies and ΔSST.</p

    The average wind stress curl (N/m<sup>3</sup>) in the Mozambique Channel estimated from ERA5 reanalysis data for March (a), June (b), September (c), and December (d) from 2010 to 2019.

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    The average wind stress curl (N/m3) in the Mozambique Channel estimated from ERA5 reanalysis data for March (a), June (b), September (c), and December (d) from 2010 to 2019.</p
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