Author: M. van EijkPublisher:
ISBN: 9789036921527
Category : Boundary layer (Meteorology)
Languages : en
Pages : 27
Book Description
The Implementation of Two Mixed-layer Schemes in the HOPE Ocean General Circulation Model
Author: M. van EijkPublisher:
ISBN: 9789036921527
Category : Boundary layer (Meteorology)
Languages : en
Pages : 27
Book Description
On embedding a mixed layer model into an ocean general circulation model
Author: S.G. ALDERSONOn Embedding a Mixed Layer Model Into an Ocean General Circulation Model
Author: S. G. AldersonTests of Mixed-layer Schemes and Surface Boundary Conditions in an Ocean General Circulation Model, Using the IMET Flux Data Set
Author: J. S. GodfreyPublisher:
ISBN: 9780643061576
Category : Electronic books
Languages : en
Pages : 39
Book Description
Research on Modeling the Oceanic General Circulation and the Surface Mixed Layer
Author: William Lawrence GatesPublisher:
ISBN:
Category : Ocean circulation
Languages : en
Pages : 260
Book Description
Biennial Scientific Report 1997-1998
Author: Koninklijk Nederlands Meteorologisch InstituutPublisher:
ISBN:
Category : Climatology
Languages : en
Pages : 164
Book Description
On Improving the Accuracy of Mixed Layer Permaterization for Ocean General Circulation Models
Author: Yuechen ZhaoParameterization of the Oceanic Mixed Layer for Use in General Circulation Models
Author: Robert C. HealdPublisher:
ISBN:
Category : Climatology
Languages : en
Pages : 48
Book Description
The behavior of different parameterizations of mixed layer physics when used in an oceanic general circulation model (OGCM) having coarse resolution of the upper ocean is examined. The method of parameterization is expected to have an important effect on the resulting sea surface temperature, and hence affect the model's overall fidelity from the viewpoint of air-sea interaction. Tests of three possible parameterizations differ in the manner in which the mixed layer depth is determined: predetermination, diagnostic determination, or prognostic determination. The sea surface temperature is taken to be equivalent to the top OGCM layer temperature in the first two methods, while it is found prognostically in the third method. Results show that for typical forcing cases such as strong insolation, weak surface cooling or weak winds, mixing is insufficient to cause heat transfer between the top two OGCM layers, which occupy the uppermost 500 m of the model. The predetermined and diagnostically determined mixed layer depth parameterizations reduce to a diffusive mixing parameterization, while the prognostic approach satisfactorily models mixed layer depths for all forcing cases. The prognostic method also agrees most closely with the results of a mixed layer model and with observations.
A general model of the ocean mixed layer
Author: Roland W. GarwoodPublisher:
ISBN:
Category : Ocean-atmosphere interaction
Languages : en
Pages : 96
Book Description
Author: