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Titlebook: Heaving, Stretching and Spicing Modes; Climate Variability Rui Xin Huang Book 2020 Higher Education Press and Springer Nature Singapore Pt

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发表于 2025-3-21 16:07:13 | 显示全部楼层 |阅读模式
书目名称Heaving, Stretching and Spicing Modes
副标题Climate Variability
编辑Rui Xin Huang
视频video
概述Provides new approaches for oceanographic study.Offers new methods in analysis of climate data.Postulates new concepts of signal analysis, including radius of signals and heaving ratio
图书封面Titlebook: Heaving, Stretching and Spicing Modes; Climate Variability  Rui Xin Huang Book 2020 Higher Education Press and Springer Nature Singapore Pt
描述.This book is focused on fundamental aspects of climate variability in the ocean, in particular changes of the wind-driven circulation. The vertical movement of isopycnal (isothermal) layers, including their stretching and compression, is called heaving and stretching. A major part of climate variability in the ocean is heaving in nature. Heave is primarily associated with the adiabatic motions of isopycnal layers due to change of wind stress. It is rather difficult to separate the contributions from adiabatic and diabatic processes..Isopycnal analysis has been widely used in climate study; however, it is much more accurate to study the isopycnal layers. Here climate signals are examined in terms of changes of layer depth, layer thickness, layer temperature/salinity, spicity and others..In addition to the traditional Theta-S diagram, the sigma-pi (potential density – potential spicity) diagram can also be used in analyzing water mass property distribution and climatevariability. In fact, a radius of signal can be defined rigorously for signals in the sigma-pi diagram; the combination of isopycnal analysis and evaluation of radius of signal provides a powerful tool in analyzing clim
出版日期Book 2020
关键词Climate change and the ocean; Thermohaline circulation; Heaving motions; global warming Hiatus; Isopycna
版次1
doihttps://doi.org/10.1007/978-981-15-2941-2
isbn_softcover978-981-15-2943-6
isbn_ebook978-981-15-2941-2
copyrightHigher Education Press and Springer Nature Singapore Pte Ltd. 2020
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978-981-15-2943-6Higher Education Press and Springer Nature Singapore Pte Ltd. 2020
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Climate Variability Diagnosed from the Spherical Coordinates,, in the first part of this chapter we examine the climate variability using the .-coordinate; at the end of this chapter, we will also explore using longitudinal and latitudinal coordinates to diagnose the climate variability.
发表于 2025-3-22 20:11:51 | 显示全部楼层
Heaving, Stretching, Spicing and Isopycnal Analysis,r can be further separated into three basic terms: anomalies in momentum, heat and freshwater fluxes through the air-sea interface. Tidal dissipation anomalies can also induce climate variability; however, such variability is characterized by much longer time scales, and thus will not be discussed here.
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Basic Concepts,s driven by surface thermohaline forcing. However, in the new paradigm the oceanic circulation is a dissipation system, maintenance of which requires external sources of the mechanical energy from the wind and the tidal dissipation.
发表于 2025-3-23 09:35:43 | 显示全部楼层
Climate Variability Diagnosed from the Spherical Coordinates,, in the first part of this chapter we examine the climate variability using the .-coordinate; at the end of this chapter, we will also explore using longitudinal and latitudinal coordinates to diagnose the climate variability.
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