2010
DOI: 10.5194/angeo-28-677-2010
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Reply to Comment on "Global structure, seasonal and interannual variability of the migrating semidiurnal tide seen in the SABER/TIMED temperatures (2002–2007)" by Manson et al. (2010)

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Cited by 8 publications
(3 citation statements)
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“…Other modes, like the antisymmetric (1, 2), (2, 3), (2, 5), (3, 4), and (3, 6) modes, also make considerable contributions to the corresponding components. These results are in agreement with the previous works [ Chang and Avery , ; Guharay and Franke , ; Mukhtarov et al ., ; Oberheide et al ., ; Pancheva et al ., ; Xue et al ., ; Yuan et al ., ].…”
Section: Data Analysis and Resultsmentioning
confidence: 99%
“…Other modes, like the antisymmetric (1, 2), (2, 3), (2, 5), (3, 4), and (3, 6) modes, also make considerable contributions to the corresponding components. These results are in agreement with the previous works [ Chang and Avery , ; Guharay and Franke , ; Mukhtarov et al ., ; Oberheide et al ., ; Pancheva et al ., ; Xue et al ., ; Yuan et al ., ].…”
Section: Data Analysis and Resultsmentioning
confidence: 99%
“…SABER diagnostics using 60‐day running mean Fourier fits indicates ≥10‐K amplitude of the semidiurnal tide at altitudes ≥100 km in the 20–40° latitude range between April and September in the Southern Hemisphere and October to March in the Northern Hemisphere, respectively, but comparatively small (≤5 K) amplitudes equatorward of 20° (e.g., Akmaev et al, ). Note that semidiurnal tidal amplitudes decrease rapidly toward lower altitudes at all latitudes, that is, ≤5 K in the 20–40° latitude range at 90 km (Pancheva et al, ). Equation suggests that the semidiurnal aliasing can be estimated as the semidiurnal amplitude times sin()π6t.…”
Section: Model and Sabermentioning
confidence: 98%
“…These waves profoundly affect the large‐scale dynamics of the mesosphere and lower thermosphere (MLT) where they attain large amplitudes and dominate the large‐scale atmospheric fields. Recent studies based on the observations made by the Sounding of the Atmosphere using Broadband Emission Radiometry (SABER) and the TIMED Doppler Interferometer (TIDI) instruments on the Thermosphere‐Ionosphere‐Mesosphere‐Energetics and Dynamics (TIMED) satellite have provided new insight into tidal fields and revealed the global distribution and climatology of the most important tidal components in temperature and neutral winds respectively [e.g., Zhang et al , 2006; Huang et al , 2006a, 2006b; Forbes et al , 2006; Oberheide et al , 2007; Oberheide and Forbes , 2008; Mukhtarov et al , 2009; Xu et al , 2009; Pancheva et al , 2009a, 2010a; Pancheva and Mukhtarov , 2011a]. Some of the above mentioned studies clearly suggested that the nonmigrating tides are much larger than previous anticipated and often exceed the migrating tide counterparts in the lower thermosphere [e.g., Zhang et al , 2006; Forbes et al , 2006, 2008; Oberheide et al , 2006, 2007; Pancheva et al , 2009b, 2010b].…”
Section: Introductionmentioning
confidence: 99%