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Marine Geological and Geophysical Roots of the Ocean OBservatories Initiative

机译:海洋观测倡议海洋地质和地球物理根源

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摘要

The ocean sciences are based on a rich exploratory heritage that dates back over a century, and expeditionary oceanography on dedicated research vessels will remain a vital component of current ocean sciences research―but a complementary new approach is also being embraced by the ocean sciences community. Recent decades have witnessed increasingly detailed spatial exploration of the oceans and seafloor, along with an evolution toward temporal exploration of change in the oceans and linkages among active processes through sustained time-series observations and adaptive long-term observatory technology. Understanding temporal evolution and linkages among processes in the oceans and the underlying plates will require a coordinated investment in a full-time observational presence within the oceans and on and beneath the seafloor―an approach that is embodied in the budding Ocean Observatories Initiative (OOI) and Ocean Research Interactive Observatories Network (ORION) program within the National Science Foundation (NSF; Isern and Clark, in press; Clark, foreword to this volume). While the value of sustained time series observations is acknowledged throughout all ocean sciences, some of the earliest coordinated efforts toward seafloor observatory science came from marine geology and geophysics, either within formal programs or from small groups of scientists. The purpose of this article is to provide a brief historical perspective of the marine geological and geophysical roots that have joined with comparable roots from other branches of ocean sciences (described in other articles in this issue) in the evolutionary process toward ocean and seafloor observatory science. The philosophical approach and investments in infrastructure for sustained time-series observations can be shared across all disciplines of ocean sciences, and ultimately, crossing the lines between disciplines may be one of the greatest benefits of the OOI.
机译:海洋科学建立于一个世纪以前的丰富探索性遗产基础之上,专门研究船上的远洋海洋学将仍然是当前海洋科学研究的重要组成部分,但是海洋科学界也正在接受一种补充性的新方法。近几十年来,对海洋和海底的空间探索越来越详细,并且通过持续的时间序列观测和适应性的长期观测技术向海洋变化的时空探索和活动过程之间的联系演变而来。要了解海洋及其底层板块之间的时间演化和联系,就需要在海洋内部以及在海底之上和之下的全时观测活动中进行协调性投资,这是在萌芽的海洋观测倡议(OOI)中体现的一种方法。美国国家科学基金会(NSF; Isern和Clark,印刷中; Clark,该卷的前言)中的海洋研究互动天文台网络(ORION)计划。尽管持续时间序列观测的价值在所有海洋科学中都得到了认可,但在海底观测科学方面的一些最早的协调努力却来自海洋地质和地球物理学,无论是在正式计划中还是在小组科学家中。本文旨在提供有关海洋地质和地球物理根源的简要历史观点,这些根源与海洋科学其他分支的可比根源(在本期其他文章中有所描述)在朝着海洋和海底观测科学的进化过程中相结合。可以在海洋科学的所有学科之间共享用于进行持续时间序列观测的基础设施的哲学方法和投资,最终,跨越学科之间的界线可能是OOI的最大好处之一。

著录项

  • 来源
    《Oceanography》 |2003年第4期|p.6-11|共6页
  • 作者

    Keir Becker;

  • 作者单位

    Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, Florida USA;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 海洋学;
  • 关键词

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