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Surface dispersion in the Gulf of California

机译:加利福尼亚湾的表面扩散

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Surface dispersion is measured in the Gulf of California by means of Argos drifters released along this semi-enclosed, elongated basin. First, basic one-particle statistics (Lagrangian scales, absolute dispersion and diffusion coefficients) are estimated along and across the Gulf. Absolute dispersion shows a nearly ballistic regime during the Lagrangian time scale (<2 days) in both directions (it grows as similar to t(2), where t is time). During the subsequent 30 days, absolute dispersion enters a random-walk regime (similar to t) along the Gulf, while being saturated across the basin due to the lateral boundaries. Secondly, the analysis is extended to two-particle statistics (relative dispersion between pairs of drifters and Finite Scale Lyapunov Exponents, FSLE). Relative dispersion is nearly exponential in both directions during the first few days, though evidence is not conclusive. During the subsequent 30 days, it grows as similar to t(1.5) along the Gulf, while being saturated across the basin again. It is shown that relative dispersion along the Gulf is proportional to <(t)over cap>(3), where (t) over cap represents a shifted time that depends on the initial separation of the particles. This form of the Richardson regime is consistently measured for particles that are sufficiently separated (30 km or more). The Richardson regime is verified with the FSLE for particle separations ranging from 30 to 140 km, approximately. The obtained dispersion properties are discussed in terms of the main circulation features within the basin, such as mesoscale vortices that occupy the width of the Gulf. These structures might retain buoys during days or weeks, thus preventing or delaying further displacements and therefore affecting the particle dispersion. The vortices are also an important mechanism to translate particles across the Gulf, between the Peninsula and the continent, thus promoting the saturation of dispersion along this direction. (C) 2015 Elsevier Ltd. All rights reserved.
机译:通过沿着这个半封闭的细长盆地释放的Argos漂移器测量加利福尼亚湾的表面扩散。首先,估算沿海湾地区和整个海湾地区的基本单粒子统计数据(拉格朗日尺度,绝对色散和扩散系数)。绝对色散在拉格朗日时间尺度(<2天)内在两个方向上都显示出几乎是弹道状态(它的增长类似于t(2),其中t是时间)。在随后的30天中,绝对扩散沿海湾进入随机游走状态(类似于t),但由于横向边界而在整个盆地上达到饱和。其次,分析扩展到两粒子统计(漂移对与有限尺度Lyapunov指数之间的相对分散,FSLE)。在头几天,相对分散在两个方向上几乎成指数增长,尽管证据尚无定论。在随后的30天中,它沿海湾的生长速度与t(1.5)相似,而整个盆地又再次达到饱和。结果表明,沿海湾的相对分散度与<(t)上限>(3)成比例,其中(t)上限表示偏移时间,该时间取决于粒子的初始分离。对于充分分离的粒子(30 km或更长),始终测量这种形式的Richardson体制。理查森政权已通过FSLE进行了约30至140 km的颗粒分离验证。根据盆地内部的主要环流特征(如占据海湾宽度的中尺度涡旋)讨论了获得的扩散特性。这些结构可能在数天或数周内保留浮标,从而防止或延迟了进一步的位移,从而影响了粒子的分散。涡旋也是使颗粒在半岛和大陆之间跨海湾移动的重要机制,从而促进了沿该方向的分散饱和。 (C)2015 Elsevier Ltd.保留所有权利。

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  • 来源
    《Progress in Oceanography》 |2015年第sepaptaa期|24-37|共14页
  • 作者

    Sanson L. Zavala;

  • 作者单位

    CICESE, Dept Phys Oceanog, Mexico City, DF, Mexico.;

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  • 正文语种 eng
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