Wave interactions. Describing waves A crest represents all the high points in a wave. A trough is all the low points in the wave.
Essential idea: When traveling waves meet they can superpose to form standing waves in which energy may not be transferred. Nature of science: Common.
The 3rd International Workshop on Next Generation Climate Models for Advanced High Performance Computing Facilities Tokyo, Japan, March 28 -30, 2001 Performance.
The Schoolwide Applications Model (SAM) An RtI-Driven Approach to School Reform Wayne Sailor University of Kansas For Professional Development Conference.
Analysis of four decadal simulations of the Skagerrak mesoscale circulation using two ocean models Lars Petter Røed 1 and Jon Albretsen 2 Presented at.
NOAA/NOS/OCS/Coast Survey Development Laboratory Lyon Lanerolle 1,2, Richard Patchen 1 and Frank Aikman III 1 1 National Oceanic and Atmospheric Administration.
NASA ROSES – Interdisciplinary Research in Earth Science (IDS) Linking Greenland ice sheet mass loss to decadal circulation changes in the ocean and atmosphere.
Primitive equation models These are the most sophisticated type of ocean circulation model, including more of the physics than the analysis systems and.
Predictability of Japan / East Sea (JES) System to Uncertain Initial / Lateral Boundary Conditions and Surface Winds LCDR. Chin-Lung Fang LCDR. Chin-Lung.
1 Atmospheric dynamics of red supergiant stars Andrea Chiavassa Groupe de Recherche en Astronomie et Astrophysique du Languedoc GRAAL Thesis advisor: Bertrand.
A Simple Model for Oxygen Dynamics in Chesapeake Bay Malcolm Scully 1)Background and Motivation 2)Simplified Modeling Approach 3)Importance of Physical.
Coupled Ocean-Atmosphere model for Regional Climate studies in the Mediterranean Sea William Cabos Departamento de Física Universidad de Alcalá European.