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Mapping ocean mixing using autonomous gliders: Indian Ocean and Antarctic shelf seas

使用自主滑翔机绘制海洋混合图：印度洋和南极陆架海

基本信息

批准号：
1942133
负责人：
金额：
--
依托单位：
University of East Anglia
依托单位国家：
英国
项目类别：
Studentship
财政年份：
2017
资助国家：
英国
起止时间：
2017 至无数据
项目状态：
已结题

来源：
https://gtr.ukri.org/projects?ref=studentship-1942133
关键词：
Mapping ocean mixing using autonomous

项目摘要

Project Rationale:How much turbulent mixing occurs in the ocean and where this mixing takes place is one of the key unanswered questions in physical oceanography. Direct measurements of turbulence at a limited number of locations appear to underestimate the background level of mixing relative to indirect estimates based on an advective-diffusive balance between global mean stratification and global upwelling. It is clear that mixing does not occur uniformly throughout the ocean interior, but as a community we are far from identifying all the global "hotspots" of mixing. The spatial distribution is of particular importance because mixing and associated sub-gridscale processes have to be parameterised in large-scale ocean circulation and climate models, typically as a spatially uniform diffusivity. However, it has been shown that predictions from such models can be sensitive to where mixing is enhanced. A better understanding of the spatial distribution (and temporal variability) of turbulent mixing in the ocean is therefore essential for development of realistic mixing parameterisations. This project will use new and existing measurements of turbulence collected using autonomous ocean gliders, along with recently developed and established analysis methods, to investigate the spatial distribution and temporal variability of turbulent mixing in multiple areas of the global ocean.Methodology:The student will use high-resolution temperature data from microstructure gliders, along with standard temperature/salinity measurements collected by these and other gliders, to make estimates of turbulent mixing rate. As part of the wider project, independent estimates of mixing rate will be made using microstructure shear data following the methods of Fer et al. (2014) and Palmer et al. (2015). These will be used for cross-validation. Specific objectives for this PhD project are:1) Make estimates of turbulent kinetic energy (TKE) dissipation rate and diapycnal eddy diffusivity in Loch Linnhe, the Indian Ocean, and around the West Antarctic Peninsula from the fast-response thermistor data using the method of Peterson and Fer (2014) and Thorpe scale analysis.2) Compare these mixing rates with those inferred from the standard temperature/salinity measurements using the large eddy method.3) Identify regions and periods of energetic mixing then, depending on the interests of the student, investigate either: (a) the dynamical processes that drive the mixing, for example internal waves, using advanced analysis methods; or (b) the effect of the mixing on local ocean chemistry and phytoplankton populations using additional data from the biogeochemical sensors on the gliders.Training:The NEXUSS CDT provides state-of-the-art, highly experiential training in the application and development of cutting-edge Smart and Autonomous Observing Systems for the environmental sciences, alongside comprehensive personal and professional development. There will be extensive opportunities for students to expand their multi-disciplinary outlook through interactions with a wide network of academic, research and industrial / government / policy partners. The student will be registered at University of East Anglia (UEA), and hosted at UEA School of Environmental Sciences. The student will join both the UEA Glider Science Group (www.ueaglider.uea.ac.uk) and the BAS Glider Group. Specific training will include: - Autonomous ocean glider data processing, quality control, and analysis techniques - Microstructure data processing and analysis techniques- Ocean glider operations, including preparation, deployment, and piloting- Participation in oceanographic research cruises- Numerical modelling of dynamic ocean processes - Presentation of research at international conferences and workshops

项目原理：海洋中发生了多少湍流混合以及这种混合发生在哪里是物理海洋学中未解决的关键问题之一。相对于基于全球平均分层和全球上升流之间的平流-扩散平衡的间接估计，在有限数量地点对湍流的直接测量似乎低估了混合的背景水平。很明显，混合并不是均匀地发生在整个海洋内部，但作为一个群体，我们远没有确定所有全球混合的“热点”。空间分布特别重要，因为混合和相关的亚网格尺度过程必须在大尺度海洋环流和气候模式中参数化，通常是空间均匀扩散。然而，已经证明，这种模型的预测对混合增强的地方很敏感。因此，更好地了解海洋中湍流混合的空间分布（和时间变异性）对于实际混合参数化的发展至关重要。该项目将使用自主海洋滑翔机收集的新的和现有的湍流测量数据，以及最近开发和建立的分析方法，研究全球海洋多个区域湍流混合的空间分布和时间变化。方法：学生将使用来自微结构滑翔机的高分辨率温度数据，以及由这些和其他滑翔机收集的标准温度/盐度测量数据，来估计湍流混合率。作为更广泛项目的一部分，将按照Fer等人（2014）和Palmer等人（2015）的方法，使用微观结构剪切数据对混合速率进行独立估计。这些将用于交叉验证。本博士项目的具体目标是：1)利用Peterson and Fer（2014）的方法和Thorpe尺度分析，利用快速响应热敏电阻数据估算林河湖、印度洋和南极半岛西部周围的湍流动能（TKE）耗散率和湍动涡扩散率。2)将这些混合速率与使用大涡法从标准温度/盐度测量中推断的混合速率进行比较。3)确定能量混合的区域和周期，然后根据学生的兴趣，研究：(a)驱动混合的动力学过程，例如内波，使用先进的分析方法；或(b)混合对当地海洋化学和浮游植物种群的影响，使用滑翔机上的生物地球化学传感器的附加数据。培训：NEXUSS CDT为环境科学的尖端智能和自主观测系统的应用和开发提供最先进的，高度经验的培训，以及全面的个人和专业发展。通过与广泛的学术、研究和工业/政府/政策合作伙伴网络的互动，学生将有广泛的机会扩展他们的多学科视野。该学生将在东安格利亚大学注册，并在东安格利亚大学环境科学学院学习。该学生将加入东英吉利大学滑翔机科学小组（www.ueaglider.uea.ac.uk）和BAS滑翔机小组。具体培训将包括：-自主海洋滑翔机数据处理、质量控制和分析技术-微观结构数据处理和分析技术-海洋滑翔机操作，包括准备、部署和驾驶-参与海洋研究巡航-海洋动态过程的数值模拟-在国际会议和研讨会上发表研究成果