Using vertical phase differences to better resolve 3D gravity wave structure

Corwin J. Wright, Neil P. Hindley, M. Joan Alexander, Laura A. Holt, Lars Hoffmann

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5 Citations (SciVal)

Abstract

Atmospheric gravity waves (GWs) are a critically important dynamical mechanism in the terrestrial atmosphere, with significant effects on weather and climate. They are geographically ubiquitous in the middle and upper atmosphere, and thus, satellite observations are key to characterising their properties and spatial distribution. Nadir-viewing satellite instruments characterise the short horizontal wavelength portion of the GW spectrum, which is important for momentum transport; however, these nadir-sensing instruments have coarse vertical resolutions. This restricts our ability to characterise the 3D structure of these waves accurately, with important implications for our quantitative understanding of how these waves travel and how they drive the atmospheric circulation when they break. Here, we describe, implement and test a new spectral analysis method to address this problem. This method is optimised for the characterisation of waves in any three-dimensional data set where one dimension is of coarse resolution relative to variations in the wave field, a description which applies to GW-sensing nadir-sounding satellite instruments but which is also applicable in other areas of science. We show that our new "2D+1 ST"method provides significant benefits relative to existing spectrally isotropic methods for characterising such waves. In particular, it is much more able to detect regional and height variations in observed vertical wavelength and able to properly characterise extremely vertically long waves that extend beyond the data volume.

Original languageEnglish
Pages (from-to)5873-5886
Number of pages14
JournalAtmospheric Measurement Techniques
Volume14
Issue number9
DOIs
Publication statusPublished - 31 Aug 2021

Bibliographical note

Funding Information:
Acknowledgements. Corwin J. Wright was supported by a Royal Society University Research Fellowship (grant no. UF160545) and NERC (grant nos. NE/R001391/1 and NE/S00985X/1). Neil P. Hindley was also supported by the latter two grants. M. Joan Alexander and Laura A. Holt were supported, in part, by the Wave-induced Atmospheric Variability Enterprise (WAVE), a NASA Heliophysics DRIVE Science Center (grant no. 80NSSC20K0628) and by NASA (grant no. 80NSSC18K0069). Laura A. Holt was further supported by NASA (grant no. 80NSSC18K0768). We also acknowledge the vital underpinning discussions at and within the context of the “New Quantitative Constraints on Orographic Gravity Wave Stress and Drag”, an international team project supported by the International Space Science Institute, and during an NorthWest Research Associates (NWRA)-funded visit to Boulder, Colorado, by Corwin J. Wright to collaborate on developing an initial approach with M. Joan Alexander and Laura A. Holt.

Funding Information:
Financial support. This research has been supported by the Natu-

Publisher Copyright:
© Author(s) 2021.

ASJC Scopus subject areas

  • Atmospheric Science

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