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Accurate approximations for planetary and gravity waves in a polar basin Cover

Accurate approximations for planetary and gravity waves in a polar basin

Open Access
|Jan 2019

Figures & Tables

Fig. 1.

Schematic of the spherical polar co-ordinate system showing the unit vectors k^, θ̂ and φ̂ that form a right-handed triad.

Table 1.

Parameter values used by LeBlond (1964) and WPA17.

SymbolVariable (unit)ValueΩAngular velocity of Earth (s1)7.292×105RRadius of Earth (m)6.370×106gGravitational acceleration (ms2)9.8HDepth of the basin (m)5753θBColatitude of the boundary (o)12.92
Table 2.

Summary of calculated results for the frequencies of the planetary waves corresponding to azimuthal wavenumbers m=1,2 and –3. In the second and third columns are listed the frequencies given by numerical solutions of the full problem (4)–(5) and by the IT solution derived by evaluating all coefficients in (4) with θ=12θB. In the remaining columns are listed the percentage errors in the IT solution (EIT) and the asymptotic result (6 b) taken to one, two and three terms (E1E3).

(m, n)Numerical sol. of eq. (4)WPA17 IT solutionEIT (%)E1 (%)E2 (%)E3 (%)(–1, 1)3.291 × 10–33.253 × 10–31.1535.2420.3321.87 × 10–2(–1, 2)1.017 × 10–31.125 × 10–310.551.5570.0481.27 × 10–3(–1, 3)4.88 × 10–45.38 × 10–410.270.7390.0173.26 × 10–4(–1, 4)2.85 × 10–43.11 × 10–4 8.950.4310.0091.39 × 10–4(–2, 1)3.740 × 10–33.670 × 10–31.8793.0920.1466.02 × 10–3(–2, 2)1.419 × 10–31.775 × 10–325.101.1510.0327.22 × 10–4(–2, 3)7.49 × 10–49.54 × 10–427.400.6040.0132.28 × 10–4(–2, 4)4.63 × 10–45.79 × 10–425.060.3730.0071.08 × 10–4(–3, 1)3.667 × 10–33.191 × 10–312.982.2040.0883.00 × 10–3(–3, 2)1.586 × 10–31.971 × 10–324.280.9440.0244.92 × 10–4(–3, 3)8.96 × 10–41.204 × 10–334.390.5310.0111.77 × 10–4(–3, 4)5.78 × 10–47.79 × 10–434.890.3420.0068.9 × 10–5
Fig. 2.

The form of the leading order eigenfunction F0(X) given by solution (8) and normalised so as to have maximum value unity. The left panel shows the form of F0(X) for n = 1 and M = 1 (leftmost curve), 2, 3 and 4 (rightmost curve). In the right panel is shown F0(X) with M = 1 and n=1,,4 with the nth mode having n – 1 interior zeros.

Table 3.

Summary of calculated results for gravity wave frequencies for azimuthal wavenumbers m=±1, ±2 and ±3. The second and third columns give the numerically determined values using the full equation and the IT approximation. Remaining columns list the predicted frequencies using the two and three term series taken from (24) and their respective associated errors.

(m, n)Numerical sol. of equation (4)WPA17 IT solutionTwo-term asymptoteError (%)Three-term asymptoteError (%)(–1, 1)2.58732.94592.50643.1282.59240.197(–1, 2)6.16405.81866.08251.3236.16670.044(–1, 3)9.74619.19129.69440.5319.74710.011(1, 1)1.75562.38601.66954.9001.75560.001(1, 2)6.09255.74086.00961.3616.09380.022(1, 3)9.71839.16099.66660.5339.71930.011(–2, 1)3.90144.93853.83901.6003.90670.137(–2, 2)7.72287.04607.65380.8937.72490.028(–2, 3)11.378410.01111.32670.41511.37470.008(2, 1)3.15854.59553.08832.2233.15600.078(2, 2)7.62636.94007.55620.9207.62730.013(2, 3)11.33199.958611.28470.41611.33280.008(–3, 1)5.16917.09065.11111.1235.17490.111(–3, 2)9.20758.69699.14380.6919.20930.020(–3, 3)12.937411.23512.89170.35312.93820.006(3, 1)4.48486.85104.41751.5014.48120.079(3, 2)9.09998.59299.03520.7109.10070.009(3, 3)12.887311.17312.84160.35512.88810.006
Fig. 3.

The form of the leading order eigenfunction F˜0(X) given by solution (19) and normalised so as to have maximum value unity. The left panel shows the form of F˜0(X) for n = 1 and |m|=1 (leftmost curve), 2, 3 and 4 (rightmost curve). In the right panel is shown F˜0(X) with |m|=1 and n=1,,4 with the nth mode having n – 1 interior zeros.

Language: English
Page range: 1618133 - 1618133
Published on: Jan 1, 2019
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services

© 2019 Andrew P. Bassom, Andrew J. Willmott, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.