Final Report I
Final Report I
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In our eReader you can find the full English version of the book. Read Final Report I Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book Final Report I
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2. The Mathematical Model, Coefficient of Friction, Zonal Flow, Basic Climatological Flow The two-dimensional flow of an inviscid, incompressible fluid layer, for which the hydrostatic approximation is made and which is subject to friction as it moves over a perfectly spherical earth of radius a, is governed by two equations for the tangential components of velocity, u and v: (2. 1) ^ u - (f + H tan e)v + ^-^^ ^ + ^^^ = o, (2o2) • ^ V + (f + I tan 0)u + I 1^ + Rvq =, where _D_ ^ ^ u ^ + Z ^ . D...t "St a cos e "Sa a. W ' and the equation of continuity for the free surface height of the layer, h: (2. 3) |5 + ^-^ [^ (hu) + ^ (hv cos e)] = ; ^ -^ dt a cos 6 '-dA ^ ^ d© ' the system (2. 1)- (2. 3) can be represented as the homogeneous system L(W) =, where W is a vector with three components, (u, v, h). The independent variables A and 6 represent longitude and latitude respectively, with corresponding components of velocity, u and v; g is the gravi- tational constant; f = 20 sin is the Coriolis parameter, where O is the rate of angular rotation of the earth; while R is a constant coefficient so that the friction force is thus taken proportional r2~.
What to read after Final Report I?
You can find similar books in the "Read Also" column, or choose other free books by J J Stoker to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
2. The Mathematical Model, Coefficient of Friction, Zonal Flow, Basic Climatological Flow The two-dimensional flow of an inviscid, incompressible fluid layer, for which the hydrostatic approximation is made and which is subject to friction as it moves over a perfectly spherical earth of radius a, is governed by two equations for the tangential components of velocity, u and v: (2. 1) ^ u - (f + H tan e)v + ^-^^ ^ + ^^^ = o, (2o2) • ^ V + (f + I tan 0)u + I 1^ + Rvq =, where _D_ ^ ^ u ^ + Z ^ . D...t "St a cos e "Sa a. W ' and the equation of continuity for the free surface height of the layer, h: (2. 3) |5 + ^-^ [^ (hu) + ^ (hv cos e)] = ; ^ -^ dt a cos 6 '-dA ^ ^ d© ' the system (2. 1)- (2. 3) can be represented as the homogeneous system L(W) =, where W is a vector with three components, (u, v, h). The independent variables A and 6 represent longitude and latitude respectively, with corresponding components of velocity, u and v; g is the gravi- tational constant; f = 20 sin is the Coriolis parameter, where O is the rate of angular rotation of the earth; while R is a constant coefficient so that the friction force is thus taken proportional r2~.
What to read after Final Report I?
You can find similar books in the "Read Also" column, or choose other free books by J J Stoker to read onlineMoreLess
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