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Upper Atmospheric Gravity Wave Details Revealed in Nightglow Satellite Imagery

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Upper Atmospheric Gravity Wave Details Revealed in Nightglow Satellite Imagery Upper atmospheric gravity wave details revealed in nightglow satellite imagery Steven D. Millera,1, William C. Straka IIIb, Jia Yuec, Steven M. Smithd, M. Joan Alexandere, Lars Hoffmannf, Martin Setvákg, and Philip T. Partaina aCooperative Institute for Research in the Atmosphere, Colorado State University, Fort Collins, CO 80523; bCooperative Institute for Meteorological Satellite Studies, University of Wisconsin-Madison, Madison, WI 53706; cAtmospheric and Planetary Science, Hampton University, VA 23668; dCenter for Space Physics, Boston University, Boston, MA 02215; eNorthWest Research Associates/Colorado Research Associates, Boulder, CO 80301; fJülich Supercomputing Centre, Forschungszentrum Jülich, Jülich, Germany; and gCzech Hydrometeorological Institute, Satellite Department, Prague, Czech Republic Edited by Mark H. Thiemens, University of California at San Diego, La Jolla, CA, and approved October 12, 2015 (received for review April 24, 2015) Gravity waves (disturbances to the density structure of the atmo- horizontal spatial resolution to capture the full circulation, they are sphere whose restoring forces are gravity and buoyancy) comprise beginning to resolve the subgrid-scale details of mesospheric waves the principal form of energy exchange between the lower and upper (15). However, these numerical models lack the observations nec- atmosphere. Wave breaking drives the mean upper atmospheric essary to constrain and improve upon gravity wave drag parame- circulation, determining boundary conditions to stratospheric pro- terizations, resulting in possible misrepresentation of important cesses, which in turn influence tropospheric weather and climate gravity wave processes. Hence there is a clear and pressing need for patterns on various spatial and temporal scales. Despite their recog- high-resolution, global observations of the transient and episodic nized importance, very little is known about upper-level gravity wave gravity wave spectrum reaching the upper atmosphere (16). characteristics. The knowledge gap is mainly due to lack of global, Whereas satellite-based measurements have helped to construct high-resolution observations from currently available satellite observ- a global climatology of gravity waves in the middle stratosphere ing systems. Consequently, representations of wave-related processes (30–40 km), such detailed global information about waves reaching in global models are crude, highly parameterized, and poorly con- the upper mesosphere is unavailable (17, 18). The data gap has strained, limiting the description of various processes influenced by limited substantive progress in a critical area. them. Here we highlight, through a series of examples, the unantic- Here we show how the nadir-viewing Day/Night Band (DNB) ipated ability of the Day/Night Band (DNB) on the NOAA/NASA radiometer on the Suomi National Polar-orbiting Partnership Suomi National Polar-orbiting Partnership environmental satellite to (NPP; hereafter, Suomi) satellite (19) holds promise for begin- resolve gravity structures near the mesopause via nightglow emis- ning to fill this gap, offering a unique ability to resolve the fine- sions at unprecedented subkilometric detail. On moonless nights, the scale horizontal structure (at ∼0.74-km resolution) of gravity Day/Night Band observations provide all-weather viewing of waves waves near the mesopause (∼90 km) globally via sensing of as they modulate the nightglow layer located near the mesopause nocturnal atmospheric airglow (or “nightglow”; 20) emissions on (∼90 km above mean sea level). These waves are launched by a moonless nights. We present representative DNB imagery ex- variety of physical mechanisms, ranging from orography to convec- amples of waves launched by a variety of physical mechanisms: tion, intensifying fronts, and even seismic and volcanic events. Cross- isolated and organized convection, topography, jet instabilities, referencing the Day/Night Band imagery with conventional thermal and a volcanic eruption. This windfall capability arises from the infrared imagery also available helps to discern nightglow structures DNB’s extreme sensitivity to low-level light and holds potentially and in some cases to attribute their sources. The capability stands to advance our basic understanding of a critical yet poorly constrained Significance driver of the atmospheric circulation. As an unforeseen windfall of its high sensitivity, the Day/Night Suomi NPP | VIIRS | Day/Night Band | nocturnal observations | airglow Band (DNB) low-light visible sensor carried on the Suomi satellite enables global detection of gravity waves in the upper atmo- ravity waves (1) play a central role in the atmospheric cir- sphere at unprecedented subkilometric detail. On moonless – Gculation (2 4) at space and time scales ranging from re- nights, the observations provide all-weather viewing of waves as gional weather to global climate (5). The momentum imparted by they modulate the nightglow layer located near the mesopause. wave breaking modulates the upper atmospheric wind flow, which These waves are launched by a variety of mechanisms ranging in turn influences weather and climate patterns through myriad from orography to convection, intensifying fronts, and seismic coupling processes (6). Examples include the Quasi-Biennial Os- and volcanic events. Wave energy is recognized as the principal cillation, which modulates monsoonal precipitation (7) and mid- driver of upper atmospheric circulation, which in turn influences latitude storm tracks (6), the Brewer–Dobson circulation, which tropospheric weather patterns. For lack of global observations, governs stratospheric ozone transport, and the Semi-Annual Os- information about upper atmospheric wave distribution and cillation, which links to the El Niño Southern Oscillation (8) and character is limited. Here, the DNB begins to fill a critical gap. to high-latitude climatology (9). These waves also influence the formation and properties of polar stratospheric clouds (10). Wave- Author contributions: S.D.M. designed research; S.D.M. and W.C.S. performed research; S.D.M., induced disturbance of ionospheric structure (11) impacts global W.C.S., J.Y., S.M.S., M.J.A., L.H., M.S., and P.T.P. analyzed data; S.M.S. supplied Fig. S2;M.J.A. helped analyze winds for Fig. 1; L.H. provided information for Fig. 3; M.S. provided Fig. S3; positioning system (GPS) performance, linking these remote P.T.P. supported analysis of Fig. 1 and Fig. S1; W.C.S. assisted with data acquisition and primary waves to practical aspects of everyday life. figure preparation; J.Y., S.M.S., M.J.A., L.H., M.S., and P.T.P. assisted with technical review, Addressing the high uncertainties in the atmospheric circulation analysis, and supplementary information; and S.D.M. wrote the paper. response to external forcing (12) will require better abilities to The authors declare no conflict of interest. model the fully coupled system. Improved representation of gravity This article is a PNAS Direct Submission. wave forcing mechanisms, global distribution, space/time evolution, Freely available online through the PNAS open access option. and momentum deposition processes is of prime importance to 1To whom correspondence should be addressed. Email: [email protected]. middle-to-upper atmospheric circulation (13, 14). As numerical This article contains supporting information online at www.pnas.org/lookup/suppl/doi:10. models extend their upper bounds (>100 km) and increase their 1073/pnas.1508084112/-/DCSupplemental. E6728–E6735 | PNAS | Published online November 16, 2015 www.pnas.org/cgi/doi/10.1073/pnas.1508084112 Downloaded by guest on September 27, 2021 broad implications for model handling of a key atmospheric astronomically dark nights (31) from its 824-km vantage point. PNAS PLUS − − − − energy transfer process. The signals, ranging from 10 5 to 10 7 Wm 2 sr 1 (∼100 times fainter than substantially moonlit scenes) manifest both as direct Wading into the Deep End of the Atmospheric Wave Pool upwelling emission and reflection by underlying clouds and the Earth-viewing satellites provide the best means of yielding global surface. Thermal infrared window bands included on VIIRS observations of high-altitude gravity waves. Since the 1960s, provide a means for decoupling the two components. satellites have characterized gravity wave distributions in the The DNB captures the fine-scale details of gravity waves at middle atmosphere (21–23). Whereas nadir-viewing infrared unprecedentedly high horizontal spatial resolution (742 m across sounders, which offer much higher horizontal spatial resolution a 3000-km-wide swath). The sensor collects data via a whiskbroom- (∼10 km) than limb sounders and GPS radio occultation systems scanning pattern using 16 detectors, with scans oriented per- (∼100 km), have provided a global climatology of stratospheric pendicular to the direction of satellite motion. Each scan of this gravity waves, corresponding high-resolution observations of detector stack forms an ∼12-km in-track swath, and adjacent waves occurring at mesospheric levels and above have not been scans are ∼1.78 s apart. The horizontal spatial resolution of DNB available on a regular basis. imagery is maintained at a value of ∼0.74 km across the entire Nightglow offers a unique perspective on gravity waves that swath (i.e., from nadir to scan edge) via a scan-angle-dependent reach higher altitudes—with strongest emissions near the 85- to subpixel aggregation strategy. The ability of the
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