权益分类	功能权益	普通用户	{{item.name}}会员
{{category.name}}	{{benefitItem.name}}

BoBBLE: Bay of Bengal Boundary Layer Experiment

BoBBLE：孟加拉湾边界层实验

基本信息

批准号：
NE/L013800/1
负责人：
Nicholas Klingaman
金额：
$ 41.77万
依托单位：
University of Reading
依托单位国家：
英国
项目类别：
Research Grant
财政年份：
2015
资助国家：
英国
起止时间：
2015 至无数据
项目状态：
已结题

来源：
https://gtr.ukri.org/projects?ref=NE%2FL013800%2F1
关键词：
BoBBLE Bay Bengal Boundary Layer

项目摘要

The South Asian summer monsoon (June-September) provides 80% of the annual rainfall for over one billion people, many of whom depend on monsoon rains for subsistence agriculture and freshwater. It is critical to forecast accurately not only the seasonal rainfall, but also rainfall variations within the summer. Sub-seasonal "active" and "break" phases can last weeks, resulting in floods and droughts across broad areas of South Asia.Air-sea interactions are key to understanding and predicting monsoon behaviour. Ocean surface temperatures in the Bay of Bengal, east of India, remain very warm (above 28 C) throughout the summer. Evaporation from the Bay provides moisture and energy to monsoon depressions that form over the Bay and bring substantial rain to India. It is not understood how the Bay remains warm despite losing energy to these systems. Ocean temperature and salinity variations across the Bay are known to drive changes in rainfall over the Bay and surrounding land, but it is not clear how these arise or how they are maintained. This is particularly true for east-west variations in the southern Bay, a focus of this project. Although air-sea interactions are important to the monsoon, weather predictions are made with models of only the atmosphere. There is potential to improve monsoon forecasts by including well-represented air-sea interactions in models.The Bay of Bengal Boundary Layer Experiment (BoBBLE) proposes an observational campaign for the southern Bay, during the established monsoon (mid-June to mid-July). BoBBLE will deploy two ships, six ocean gliders and eight floats to collect an unprecedented range of oceanic and air-sea flux observations. The ships will occupy locations in the southwest and southeast Bay, as well as tracing east-west and north-south paths between those locations, measuring ocean temperature, salinity and currents. Two gliders (automated underwater vehicles) will accompany each ship, with two others between the ships, diving to 500 metres every 2 hours to measure temperature, salinity and currents. Diurnal variations in air-sea fluxes and ocean temperatures may affect the development of weather systems. A novel configuration of the gliders will allow computations of horizontal transports of heat and salt. The floats (automated submersibles) will be deployed in the Bay to measure the ocean to 2000 metres every 5 days. They will remain in the Bay after BoBBLE, enhancing the observing network. Ships and gliders will also measure ocean chlorophyll, which absorb sunlight and alter near-surface ocean temperature, influencing air-sea interactions.BoBBLE scientists will analyse these observations, along with routine datasets, to understand the evolution of conditions in the Bay and how they influence the atmosphere. Particular emphasis will be placed on estimating the uncertainty in existing datasets of air-sea fluxes by validating them against all available observations. The best-performing datasets will be used to improve estimates of air-sea exchanges and their variability on daily to decadal timescales, to calculate budgets of heat and freshwater fluxes in the Indian Ocean and the Bay, and to validate model simulations.A hierarchy of model simulations will reveal how conditions in the Bay are maintained and how air-sea interactions influence the monsoon. Simulations with an ocean model, forced by and validated against BoBBLE observations, will isolate the roles of air-sea fluxes (including the diurnal cycle), chlorophyll and horizontal transports in maintaining and recharging ocean structure after each weather system passage. Retrospective forecasts of the BoBBLE period with atmosphere-only and atmosphere-ocean coupled models will demonstrate how air-sea interactions influence monsoon rainfall predictions. Multi-decadal simulations will evaluate how air-sea interactions and coupled-model systematic errors influence daily-to-seasonal monsoon variability.

南亚夏季风(6-9月)为10多亿人提供了年降雨量的80%，其中许多人依靠季风雨维持农业和淡水。不仅要准确预报季节降雨量，而且要准确预报夏季降水的变化。亚季节的“活跃”和“休息”阶段可能持续数周，导致南亚大片地区的洪水和干旱。海气相互作用是了解和预测季风行为的关键。印度东部孟加拉湾的海洋表面温度在整个夏天都保持在非常温暖的(28摄氏度以上)。海湾的蒸发为海湾上空形成的季风低地提供了水分和能量，并为印度带来了大量降雨。尽管这些系统失去了能量，但海湾是如何保持温暖的，目前尚不清楚。众所周知，整个海湾的海洋温度和盐度变化会导致海湾和周围陆地上的降雨量发生变化，但目前还不清楚这些变化是如何产生的，也不清楚它们是如何维持的。南部湾的东西变化尤其如此，这是该项目的一个重点。尽管海-气相互作用对季风很重要，但天气预报只使用大气模型。通过在模式中加入具有良好代表性的海-气相互作用，有可能改进季风预报。孟加拉湾边界层实验(BOBBLE)建议在已建立的季风期间(6月中旬至7月中旬)对南湾进行观测活动。波布尔将部署两艘船、六架海洋滑翔机和八个浮标来收集前所未有的海洋和海气通量观测。这些船只将占据西南和东南湾的位置，并追踪这些位置之间的东西和南北路径，测量海洋温度、盐度和洋流。每艘船将配备两个滑翔机(自动潜水器)，两艘船之间还有两个滑翔机，每两小时潜入500米深的地方测量温度、盐度和洋流。海气通量和海洋温度的日变化可能会影响天气系统的发展。滑翔机的一种新配置将允许计算热量和盐分的水平传输。浮标(自动潜水器)将部署在海湾，每5天测量海洋2000米。他们将在一次又一次的漂浮后留在海湾，加强观测网络。船只和滑翔机还将测量海洋叶绿素，它吸收阳光，改变近表面的海洋温度，影响海-气相互作用。波士顿大学的科学家将分析这些观测结果，以及常规数据集，以了解海湾条件的演变及其如何影响大气。将特别强调通过对照所有现有的观测数据对现有的海气通量数据集进行验证，从而估计这些数据集的不确定性。表现最好的数据集将用于改进对海-气交换及其在日至年代际时间尺度上的可变性的估计，计算印度洋和海湾的热量和淡水通量的预算，并验证模式模拟。模式模拟的层次将揭示海湾的条件是如何维持的，以及海-气相互作用如何影响季风。用海洋模型进行的模拟受到气泡观测的强迫和验证，将分离出海-气通量(包括日循环)、叶绿素和水平输送在每次天气系统通过后维持和补充海洋结构方面的作用。仅使用大气和大气-海洋耦合模式对浮泡期的回顾预报将说明海气相互作用如何影响季风降雨预报。多年代际模拟将评估海-气相互作用和耦合模式系统误差如何影响逐日季风变化。