Semi-Spectral Primitive Equation Regional Ocean-Circulation Model. Version 3.0 (User's Manual).

Semi-Spectral Primitive Equation Regional Ocean-Circulation Model. Version 3.0 (User's Manual).
Author:
Publisher:
Total Pages: 94
Release: 1990
Genre:
ISBN:

This user's manual for the semi-spectral primitive equation model (SPEM) attempts to describe the model equations as well as what the user has to do to configure the model for a specific application. The principle attributes of the model are as follows: (A) General - (1) Primitive equations with temperature, salinity and an equation of state; (2) Hydrostatic and Boussinesq approximations; (3) Second-moment conservation; (4) Optional Lagrangian floats; (B) Horizontal - (1) Orthogonal-curvilinear coordinates; (2) Arakawa C grid; (3) Periodic channel or user supplied boundary conditions; and (C) Vertical - (1) Sigma(bottom-topography following) coordinate; (2) Chebyshev modal expansion, (3) Rigid lid on top.

Physics of Lakes

Physics of Lakes
Author: Kolumban Hutter
Publisher: Springer Science & Business Media
Total Pages: 660
Release: 2014-03-26
Genre: Science
ISBN: 3319004735

The ongoing thread in this volume of Physics of Lakes is the presentation of different methods of investigation for processes taking place in real lakes with a view to understanding lakes as components of the geophysical environment. It is divided into three parts. Part I is devoted to numerical modeling techniques and demonstrates that (i) wind-induced currents in depth-integrated models can only adequately predict current fields for extremely shallow lakes, and (ii) that classical multi-layered simulation models can only adequately reproduce current and temperature distributions when the lake is directly subjected to wind, but not the post-wind oscillating response. This makes shock capturing discretization techniques and Mellor-Yamada turbulence closure schemes necessary, as well as extremely high grid resolution to reduce the excessive numerical diffusion. Part II is devoted to the presentation of principles of observation and laboratory experimental procedures. It details the principles of operation for current, temperature, conductivity and other sensors applied in the field. It also discusses the advantages and limitations of common measuring methods like registration from stationary or drifting buoys, sounding and profiling from a boat, etc. Questions of data accuracy, quality, and reliability are also addressed. The use of laboratory experiments on a rotating platform is based on an exposition of dimensional analysis and model theory and illustrated using Lake Constance as an example. Part III gives an account of the dynamics of lake water as a particle-laden fluid, which, coupled with the transport of the bottom sediments, leads to morphodynamic changes of the bathymetry in estuarine and possibly whole lake regions. An elegant spatially one-dimensional theory makes it possible to derive analytic solutions of deltaic formations which are corroborated by laboratory experiments. A full three-dimensional description of the evolution of the alluvial bathymetry under prescribed tributary sediment input indicates a potential subject for future research.

The Polar Oceans and Their Role in Shaping the Global Environment

The Polar Oceans and Their Role in Shaping the Global Environment
Author: Fridtjof Nansen
Publisher: American Geophysical Union
Total Pages: 548
Release: 1994-01-10
Genre: Nature
ISBN:

Published by the American Geophysical Union as part of the Geophysical Monograph Series, Volume 85. On June 24, 1993, one hundred years had passed since Fridtjof Nansen and his companions set out on one of the most daring and exciting research expeditions the world had ever seen. They allowed their vessel, the Fram, to be frozen into the ice close to the New Siberian Islands, in the Arctic Ocean. Three years were to elapse before the ice released its hold on the Fram and allowed her to return to Norway via the strait between Greenland and Spitsbergen, which later came to be known as Fram Strait. The research carried out during Fram's drift in the ice altered forever our concept of the Arctic Basin.