03 Application study of shallow water wave model (SWAN)

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41 o 8805 8710 40 o E N 39 o 9804 38 o 118 o 119 o 120 o 121 o 122 o Figure 1 computational grid in Bohai Sea and locations of observation .
Wind processes we select four typical wind processes from historical data as following: Serial number Process Computing time Locations of stations Depth (m) 1 8710 1987.10.29 02:00—1987.11.01 02:00 120.75 o E 39.90 o N 31 2 8805 1988.05.26 08:00—1988.05.29 08:00 121.12 o E 40.208 o N 25 3 9804 1998.04.22 20:00—1998.04.25 02:00 118.817 o E 38.217 o N 10 4 9904 1999.04.18 20:00—1999.04.20 14:00 118.817 o E 38.217 o N 10 Wind fields used in this study were prepared by Ocean University of China.
Page 1 and 2: Yang dezhou Yin boshu Institute of
Page 3 and 4: Based on experiments and analysis,
Page 5 and 6: (2)Our experiments in different sea
Page 7 and 8: Linear growth by wind A = α [ U 2
Page 9 and 10: (2) Two expressions of white-cappin
Page 11 and 12: : An alternative formulation for wh
Page 13 and 14: 4. Improvement of proportionality c
Page 15 and 16: In view of the relation between Phi
Page 17 and 18: 5. Numerical implementation and res
Page 19: Computational domain All our exper
Page 23 and 24: 7 Measurements Default Komen -Alkyo
Page 25 and 26: It is easy to find out that the HS
Page 27 and 28: c: In addition, Cumulative Steepnes
Page 29 and 30: c: In addition, the amended SWAN mo
Page 31: [5] Hasselmann, K., 1974: On the sp

03 Application study of shallow water wave model (SWAN)

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