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On the determination of gravity wave momentum flux from GPS radio occultation data

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Figure

Fig. 2. Displayed are two vertical temperature profiles with a phasepoints of measurement when the corresponding horizontal wave isknown (eters (those 3 points (shift of 40◦ (a), the projected and real horizontal wavelet within 3b), the 3 points of measurem
Fig. 3. Part A of the geometrical description of the determinationand the three possible combinations of solving Eq
Fig. 5. Sensitivity study for the method introduced by Ern et al.(2004) concerning the resulting wavelength (kph ) at different hori-zontal distances and phase shifts.
Fig. 7. Horizontal wavelength (corresponding momentum fluxkph ) (a and c) and true horizontal wavelength (b) with spacings of 10◦ (a and b) and < 300 km (c) and the d − f .
+4

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