.Ocean Modelling for Beginners Phần 10 potx

... P ∂z − g  3.7 Forces 27 3.7 Forces 3.7.1 What Forces Do A non-zero force operates to change the speed and/or the direction of motion of a flui parcel. In geophysical flui dynamics, forces are conventionally ... W n |. 3.11 The Pressure-Gradient Force 3.11.1 The Hydrostatic Balance For a flui at rest, the downward acting gravity force is balanced by an upward acting pressure-gradient force...

Ngày tải lên: 23/09/2012, 14:49

... đang theo học lớp đó Bài giảng tóm tắt Hệ quản trị cơ sở dữ liệu 109 BÀI TẬP LẬP TRÌNH CƠ SỞ DỮ LIỆU Cho cơ sở dữ liệu sau (có tên tập tin cơ sở dữ liệu QLThuVien): o NhaXuatBan( MANXB , TenNXB): ... Wesley - 4th edition, 2004. [7] Sumathi, S. and Esakkirajan, S., Fundamentals of Relational Database Management Systems, Springer-Verlag, 2007. Bài giảng tóm tắt Hệ quản t...

Ngày tải lên: 11/07/2014, 15:21

... đơn vị Pico Nano Mili Micro Xenti p n m à c 10 -1 2 10 -9 10 -3 10 -6 10 -2 Deci Hecto Kilo Mega d h k xM 10 -1 100 1.000 1.000.000 171 Cấp chính xác với sai ... pha 97 Chương 5 ĐO GÓC PHA VÀ TẦN SỐ 106 5.1. Đo góc pha và hệ số công suất cosφ 106 5.2. Đo tần số 114 5.3. Ứng dụng máy hiện sóng điện tử trong đo...

Ngày tải lên: 13/07/2014, 10:22

Ngày tải lên: 13/07/2014, 10:22

Ngày tải lên: 13/07/2014, 16:20

... SampleCodeandAnimationScript 11 1 Contents xiii 5.9 Exercise 13 : Inclusion of Nonlinear Terms . . 11 1 5.9 .1 Aim 11 1 5.9.2 Formulation of the Nonlinear Terms . . . . . . 11 1 5.9.3 SampleCode 11 1 5.9.4 Results 11 2 5 .10 ... . . . 11 5 5 .10 .5 Full-Slip,Semi-SlipandNo-SlipConditions 11 5 5 .10 .6 TaskDescription 11 6 5 .10 .7 SampleCode 11 7 5 .10 .8 Results 11 7 5 .10 .9 A...

Ngày tải lên: 07/08/2014, 04:20

... (%) 0 10 100 19.090.0 28 .181.0 37 .29 72. 9 46.56 65.6 55.959.0 65.31 53.1 74.78 47.8 84.343.0 93.87 38.7 10 3.49 34.9 11 3.14 31.4 12 2. 82 28 .2 13 2. 54 25 .4 14 2. 29 22 .9 15 2. 06 20 .6 16 1.85 18.5 17 ... (−2m, −5m, 2 m) gives a new location vector (−2m, 0, −5m). The distance between two locations (x 1 , y 1 , z 1 ) and (x 2 , y 2 , z 2 ) is given by: D 2 1 =  (x...

Ngày tải lên: 07/08/2014, 04:20

... a threshold value of around 1 /4 = 0.25. Richardson (1920) was the firs to derive this instability criterion. 3. 14 Exercise 4: The Coriolis Force in Action 55 3. 14. 4 Improved Scheme 2: The Local-Rotation ... book. 3. 14 Exercise 4: The Coriolis Force in Action 3. 14. 1 Aim The aim of this exercise is to predict the pathway of a non-buoyant flui parcel in a rotating flui subject to th...

Ngày tải lên: 07/08/2014, 04:20

... Script FORTRAN simulation codes and Scilab animation scripts for both scenarios can be found in the folder “Exercise 6” of the CD-ROM. Several changes of the FORTRAN code for Exercise 5 are required ... strongly deformed owing to the axis ratio chosen Fig. 4.11 Exercise 5. Scenario 1. Same as Fig. 4.9, but with  = 0. 05 76 4 Long Waves in a Channel Fig. 4.8 Structure of the FORTRAN c...

Ngày tải lên: 07/08/2014, 04:20

... adjacent sea-level grid points J. K ă ampf, Ocean Modelling for Beginners, DOI 10.1007/978-3 -64 2-00820-7 5, C Springer-Verlag Berlin Heidelberg 2009 91 4 .6 Exercise 7: Long Waves in a Layered Fluid ... reason for wave steep- ening is that the phase speed under a wave crest exceed that under a wave trough according to (4. 16) . 5.3.7 Additional Exercise for the Reader Repeat th...

Ngày tải lên: 07/08/2014, 04:20

... steps. J. K ă ampf, Ocean Modelling for Beginners, DOI 10.10 07/ 978 -3-642-00820 -7 6, C  Springer-Verlag Berlin Heidelberg 2009 119 5.10 Exercise 14: Island Wakes 1 17 5.10 .7 Sample Code The folder ... their complete form including nonlinear terms, wind-stress forcing, the Coriolis force, the pressure-gradient force, bottom friction and lateral diffusion of momentum. The momentu...

Ngày tải lên: 07/08/2014, 04:20

... friction and is therefore governed by a balance between the horizontal pressure-gradient force and the Coriolis force – the geostrophic balance. The ocean’s dynamics can therefore be classifie by ... time it takes for a f ow of speed U to travel a distance of L. For small Rossby numbers (Ro << 1), nonlinear terms are negligibly small compared with the Coriolis force and therefore ca...

Ngày tải lên: 07/08/2014, 04:20

... are more complex and therefore not included in this book. The interested reader is referred to the work by Munk ( 195 0). 6 .9 Exercise 18: The Wind-Driven Circulation 6 .9. 1 Aim The aim of this exercise ... average 9 ◦ Celsius warmer than elsewhere for the same geographical latitude. 6 .9. 4 Sample Code and Animation Script The folder “Exercise 18” on the CD-ROM contains the computer c...

Ngày tải lên: 07/08/2014, 04:20

... 129–132 Tracer Eulerian, 104 , 106 , 107 , 109 , 111, 116, 117, 130, 131, 135, 159, 160 Lagrangian, 104 Truncation error, 10, 67–68 Turbulence, 30, 57–60, 113 TVD advection scheme, 106 , 111, 112 V Vorticity planetary, ... Pergamon Press, Oxford, 329 pp. Prandtl, L., 1925: Bericht ă uber Untersuchungen zur ausgebildeten Turbulenz, Z. Angew. Math. Mech., 5, 136139. J. K ă ampf, Ocean...

Ngày tải lên: 07/08/2014, 04:20

... mining and GVis for exploring spatio -temporal data, Proceedings ofGISRUK’98. WASSERMAN, A.I., PIRCHER, P.A. and MULLER, R.J., 1990, The object-oriented structure design for software design representation. ... Qualitative temporal reasoning in GIS ordered time scales, Proceedings of the SDH’94 Conference, Vol. 1, pp. 410 30. GARDELS, K., 1992, SEQUOIA 2000: new geographic informat...

Ngày tải lên: 07/08/2014, 04:20