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Titlebook: Stochastic Transport in Upper Ocean Dynamics II; STUOD 2022 Workshop, Bertrand Chapron,Dan Crisan,Anna Radomska Conference proceedings‘‘‘‘‘

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发表于 2025-3-21 17:12:58 | 显示全部楼层 |阅读模式
书目名称Stochastic Transport in Upper Ocean Dynamics II
副标题STUOD 2022 Workshop,
编辑Bertrand Chapron,Dan Crisan,Anna Radomska
视频video
概述This book is open access, meaning any reader has free and unlimited access.Brings selected, peer-reviewed studies in variability and uncertainty in upper ocean dynamics.Discusses means of quantifying
丛书名称Mathematics of Planet Earth
图书封面Titlebook: Stochastic Transport in Upper Ocean Dynamics II; STUOD 2022 Workshop, Bertrand Chapron,Dan Crisan,Anna Radomska Conference proceedings‘‘‘‘‘
描述This open access proceedings volume brings selected, peer-reviewed contributions presented at the Third Stochastic Transport in Upper Ocean Dynamics (STUOD) 2022 Workshop, held virtually and in person at the Imperial College London, UK, September 26–29, 2022. The STUOD project is supported by an ERC Synergy Grant, and led by Imperial College London, the National Institute for Research in Computer Science and Automatic Control (INRIA) and the French Research Institute for Exploitation of the Sea (IFREMER). The project aims to deliver new capabilities for assessing variability and uncertainty in upper ocean dynamics. It will provide decision makers a means of quantifying the effects of local patterns of sea level rise, heat uptake, carbon storage and change of oxygen content and pH in the ocean. Its multimodal monitoring will enhance the scientific understanding of marine debris transport, tracking of oil spills and accumulation of plastic in the sea..All topics of these proceedings are essential to the scientific foundations of oceanography which has a vital role in climate science. Studies convened in this volume focus on a range of fundamental areas, including:.Observations at a h
出版日期Conference proceedings‘‘‘‘‘‘‘‘ 2024
关键词Open Access; mathematics of planet earth; math open access proceedings; STUOD; ocean modelling; ocean obs
版次1
doihttps://doi.org/10.1007/978-3-031-40094-0
isbn_softcover978-3-031-40096-4
isbn_ebook978-3-031-40094-0Series ISSN 2524-4264 Series E-ISSN 2524-4272
issn_series 2524-4264
copyrightThe Editor(s) (if applicable) and The Author(s) 2024
The information of publication is updating

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Analysis of Sea Surface Temperature Variability Using Machine Learning,years. The objective is to best explain the temporal variability of the SSTA extremes. These extremes are revealed to be well explained through a non-linear interaction between multi-scale processes. The results contribute to better unveil factors influencing SSTA extremes, and the development of more accurate prediction models.
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Data Assimilation: A Dynamic Homotopy-Based Coupling Approach,h provides a computationally tractable approximation to the underlying bridge problem. In particular, our implementation builds upon the widely used ensemble Kalman filter methodology and extends it to Schrödinger bridge problems within the context of sequential data assimilation.
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Internal Tides Energy Transfers and Interactions with the Mesoscale Circulation in Two Contrasted Aposition. Two areas of interest are considered: the Azores Islands over the mid Atlantic ridge and the Gulf Stream offshore the North of the US East coast shelf break. Low mode (1 and 2) internal tides are found to propagate from 100 km (mode 2) to 1000 km (mode 1) away from their generation sites.
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Sparse-Stochastic Model Reduction for 2D Euler Equations, negligible. Solving these equations numerically can be extremely demanding. Several techniques to obtain fast and accurate simulations have been developed during the last decades. In this paper, we present a novel approach that combines recent developments in stochastic model reduction and conserva
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,Effect of Transport Noise on Kelvin–Helmholtz Instability,small-scale transport noise. As a test problem we consider the Kelvin-Helmholtz instability and we compare the inviscid case, the viscous one, both without noise, and the inviscid case perturbed by transport noise. We observe a partial similarity with the viscous case, namely a delay of the instabil
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On the 3D Navier-Stokes Equations with Stochastic Lie Transport,nd vorticity form, on the torus and the bounded domain respectively. In particular we demonstrate the efficacy of Goodair et al. (Existence and Uniqueness of Maximal Solutions to SPDEs with Applications to Viscous Fluid Equations, 2023. Stochastics and Partial Differential Equations: Analysis and Co
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On the Interactions Between Mean Flows and Inertial Gravity Waves in the WKB Approximation,nciple for the Euler–Boussinesq (EB) equations. Following Gjaja and Holm 1996, we consider 3D inertial gravity waves (IGWs) in the EB approximation. The GLM closure for WKB IGWs expresses EB wave mean flow interaction (WMFI) as WKB wave motion boosted into the reference frame of the EB equations for
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Toward a Stochastic Parameterization for Oceanic Deep Convection,quent deep convection events. We propose in this study to investigate a misrepresentation of deep convection in Hydrostatic Primitive Equation (HPE) ocean and climate models due to the lack of constraints on vertical dynamics. We discuss the potential of the Location Uncertainty (LU) stochastic repr
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