Titlebook: Ocean Wave Modeling; The SWAMP Group Book 1985 Springer Science+Business Media New York 1985 Europe.carr.earthquake prediction.evolution.m

Menthol

書目名稱Ocean Wave Modeling影響因子(影響力)




書目名稱Ocean Wave Modeling影響因子(影響力)學(xué)科排名




書目名稱Ocean Wave Modeling網(wǎng)絡(luò)公開度




書目名稱Ocean Wave Modeling網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Ocean Wave Modeling被引頻次




書目名稱Ocean Wave Modeling被引頻次學(xué)科排名




書目名稱Ocean Wave Modeling年度引用




書目名稱Ocean Wave Modeling年度引用學(xué)科排名




書目名稱Ocean Wave Modeling讀者反饋




書目名稱Ocean Wave Modeling讀者反饋學(xué)科排名

Entreaty

貞潔

978-1-4757-6057-6Springer Science+Business Media New York 1985

Emmenagogue

Decoupled Propagation ModelsThe principal characteristics of the two DP models considered in this study (. and .) are listed in Table 4.1. Details and further references can be found in the model descriptions given in Part II. For both models, wave growth is strictly decoupled up to the saturation limit.

Champion

消極詞匯

Test Strategys of individual models reveals substantial differences, even between models of the same class. In addition, the numerical implementation varies significantly from one model class to another. This raises the following questions:

Derogate

Case II: Fetch- and Duration-Limited Growthrthogonally offshore. The wind field is infinite in the lateral and downstream directions. The initial wave energy at time . = 0 is zero, and the spectrum at the coastline . = 0 remains zero for . > 0. The models were run until a stationary state was reached for the entire area.

JOG

懸掛

Summaryompared for seven test cases designed to emphasize different features of the models. The study has provided a comprehensive view of the present state of wave modeling and has revealed a number of critical areas in which further work is necessary. The principal conclusions may be summarized as follows:

Clinch

The VENICE Model for Wind Wave Prediction-water applications. We will give here only a short description of the model, particularly the part concerned with shallow-water processes. These are not of interest in the actual study because of its deep-water assumption. Readers interested in the details of the model are referred to the paper quoted.