Allison, M. (1997), Accurate analytic representations of solar time and seasons on Mars with applications to the Pathfinder/Surveyor missions, Geophys. Res. Lett., 24(16), 1967–1970, doi:10.1029/97GL01950.CrossRefGoogle Scholar

Allison, M., and McEwen, M. (2000), A post-Pathfinder evaluation of areocentric solar coordinates with improved timing recipes for Mars seasonal/diurnal climate studies, Planet. Space Sci., 48(2–3), 215–235, doi:10.1016/S0032-0633(99)00092-6.Google Scholar

Anderson, D.L.T. (1976), The low-level jet as a western boundary current, Mon. Wea. Rev., 104, 907–921, doi:10.1175/1520-0493(1976)104<0907:TLLJAA>2.0.CO;2.Google Scholar

Anderson, E., and Leovy, C.B. (1978), Mariner 9 television limb observations of dust and ice hazes on Mars, J. Atmos. Sci., 35, 723–734, doi:10.1175/1520-0469(1978)035<0723:MTLOOD>2.0.CO;2.2.0.CO;2>CrossRefGoogle Scholar

Andrews, D.G., and McIntyre, M.E. (1976), Planetary waves in horizontal and vertical shear: the generalized Eliassen–Palm relation and the mean zonal acceleration, J. Atmos. Sci., 33(11), doi:10.1175/1520-0469(1976)033<2031:PWIHAV>2.0.CO;2.Google Scholar

Andrews, D.G., Taylor, F.W., and McIntyre, M.E. (1987), The influence of atmospheric waves on the general circulation of the middle atmosphere [and discussion], Philos. Trans. R. Soc. A Math. Phys. Eng. Sci., 323(1575), 693–705, doi:10.1098/rsta.1987.0115.Google Scholar

Angelats i Coll, M., Forget, F., López-Valverde, M.A., and González-Galindo, F. (2005), The first Mars thermospheric general circulation model: the Martian atmosphere from the ground to 240 km, Geophys. Res. Lett., 32, L04201, doi:10.1029/2004GL021368.Google Scholar

Banfield, D., Ingersoll, A.P., and Keppenne, C.L. (1995), A steady-state Kalman filter for assimilating data from a single polar orbiting satellite, J. Atmos. Sci., 52, 737–753, doi:10.1175/1520-0469(1995)052<0737:ASSKFF>2.0.CO;2.Google Scholar

Banfield, D., Toigo, A.D., Ingersoll, A.P., and Paige, D.A. (1996), Martian weather correlation length scales, Icarus, 119(1), 130–143, doi:10.1006/icar.1996.0006.Google Scholar

Banfield, D., Conrath, B.J., Pearl, J.C., Smith, M.D., and Christensen, P.R. (2000), Thermal tides and stationary waves on Mars as revealed by Mars Global Surveyor Thermal Emission Spectrometer, J. Geophys. Res., 105(E4), 9521, doi:10.1029/1999JE001161.CrossRefGoogle Scholar

Banfield, D., Conrath, B.J., Smith, M.D., Christensen, P.R., and Wilson, R.J. (2003), Forced waves in the Martian atmosphere from MGS TES nadir data, Icarus, 161(2), 319–345, doi:10.1016/S0019-1035(02)00044-1.Google Scholar

Banfield, D., Conrath, B.J., Gierasch, P.J., Wilson, R.J., and Smith, M.D. (2004), Traveling waves in the Martian atmosphere from MGS TES nadir data, Icarus, 170(2), 365–403, doi:10.1016/j.icarus.2004.03.015.Google Scholar

Barnes, J.R. (1980), Time spectral analysis of midlatitude disturbances in the Martian atmosphere, J. Atmos. Sci., 37, 2002–2015, doi:10.1175/1520-0469(1980)037<2002:TSAOMD>2.0.CO;2.Google Scholar

Barnes, J.R. (1981), Midlatitude disturbances in the Martian atmosphere: a second Mars year, J. Atmos. Sci., 38, 225–234, doi:10.1175/1520-0469(1981)038<0225:MDITMA>2.0.CO;2.Google Scholar

Barnes, J.R. (1983), Baroclinic waves in the atmosphere of Mars: observations, linear instability, and finite-amplitude evolution, Ph.D Thesis, University of Washington, Seattle, Washington.Google Scholar

Barnes, J.R. (1984), Linear baroclinic instability in the Martian atmosphere, J. Atmos. Sci., 41, 1536–1550, doi:10.1175/1520-0469(1984)041<1536:LBIITM>2.0.CO;2.Google Scholar

Barnes, J.R. (1986), Finite-amplitude behavior of a single baroclinic wave with multiple vertical modes: effects of thermal damping, J. Atmos. Sci., 43, 58–71, doi:10.1175/1520-0469(1986)043<0058:FABOAS>2.0.CO;2Google Scholar

Barnes, J.R. (1990), Possible effects of breaking gravity waves on the circulation of the middle atmosphere of Mars, J. Geophys. Res., 95(B2), 1401, doi:10.1029/JB095iB02p01401.Google Scholar

Barnes, J.R. (2001), Asynoptic fourier transform analyses of MGS TES data: transient baroclinic eddies, Bull. Am. Met. Soc., 33, 1067.Google Scholar

Barnes, J.R. (2003a), Planetary eddies in the Martian atmosphere: FFSM analysis of TES data, First Int. Workshop Mars Atmos. Model. Obs., Granada, Spain, http://www-mars.lmd.jussieu.fr/granada2003/.Google Scholar

Barnes, J.R. (2003b), Mars weather systems and maps: FFSM analyses of MGS TES temperature data, Sixth Int. Conf. Mars, Pasadena, California, www.lpi.usra.edu/meetings/sixthmars2003/abstractvolume.html.Google Scholar

Barnes, J.R. (2006), FFSM studies of transient eddies in the MGS TES temperature data, Second Int. Workshop Mars Atmos. Model. Obs., Granada, Spain, http://www-mars.lmd.jussieu.fr/granada2006/.Google Scholar

Barnes, J.R., and Haberle, R.M. (1996), The Martian zonal-mean circulation: angular momentum and potential vorticity structure in GCM simulations, J. Atmos. Sci., 53, 3143–3156, doi:10.1175/1520-0469(1996)053<3143:TMZMCA>2.0.CO;2.2.0.CO;2>CrossRefGoogle Scholar

Barnes, J.R., and Hollingsworth, J.L. (1987), Dynamical modeling of a planetary wave mechanism for a Martian polar warming, Icarus, 71, 313–334.CrossRefGoogle Scholar

Barnes, J.R., and Tyler, D. (2007), Winter weather on Mars: the unique southern hemisphere, in Seventh Int. Conf. Mars, Pasadena, California, www.lpi.usra.edu/meetings/7thmars2007/.Google Scholar

Barnes, J.R., Pollack, J.B., Haberle, R.M., et al. (1993), Mars atmospheric dynamics as simulated by the NASA Ames General Circulation Model: 2. Transient baroclinic eddies, J. Geophys. Res., 98(E2), 3125–3148, doi:10.1029/92JE02935.Google Scholar

Barnes, J.R., Walsh, T.D., and Murphy, J.R. (1996a), Transport timescales in the Martian atmosphere: general circulation model simulations, J. Geophys. Res., 101(E7), 16881, doi:10.1029/96JE00500.CrossRefGoogle Scholar

Barnes, J.R., Haberle, R.M., Pollack, J.B., Lee, H., and Schaeffer, J. (1996b), Mars atmospheric dynamics as simulated by the NASA Ames General Circulation Model: 3. Winter quasi-stationary eddies, J. Geophys. Res., 101, 12753–12776.Google Scholar

Barnes, J.R., Rucker, M.S., and Tyler, D. (2014), Transient eddies in the atmosphere of Mars: the crucial importance of water clouds, in Eighth Int. Conf. Mars, Pasadena, California, www.hou.usra.edu/meetings/8thmars2014/.Google Scholar

Basu, S., Wilson, J., Richardson, M., and Ingersoll, A.P. (2006), Simulation of spontaneous and variable global dust storms with the GFDL Mars GCM, J. Geophys. Res., 111(E9), E09004, doi:10.1029/2005JE002660.Google Scholar

Benson, J.L., Kass, D.M., Kleinböhl, A., et al. (2010), Mars’ south polar hood as observed by the Mars Climate Sounder, J. Geophys. Res., 115(E12), E12015, doi:10.1029/2009JE003554.CrossRefGoogle Scholar

Blumsack, S.L. (1971), On the effects of topography on planetary atmospheric circulation, J. Atmos. Sci., 28, doi:10.1175/1520-0469(1971)028<1134:OTEOTO>2.0.CO;2.Google Scholar

Blumsack, S.L., and Gierasch, P.J. (1972), Mars: the effects of topography on baroclinic instability, J. Atmos. Sci., 29, doi:10.1175/1520-0469(1972)029<1081:MTEOTO>2.0.CO;2.Google Scholar

Blumsack, S.L., Gierasch, P.J., and Wessel, W.R. (1973), An analytical and numerical study of the Martian planetary boundary layer over slopes, J. Atmos. Sci., 30, doi:10.1175/1520-0469(1973)030<0066:AAANSO>2.0.CO;2.Google Scholar

Bougher, S.W., Engel, S., Hinson, D.P., and Forbes, J.M. (2001), Mars Global Surveyor radio science electron density profiles: neutral atmosphere implications, Geophys. Res. Lett., 28(16), 3091–3094, doi:10.1029/2001GL012884.CrossRefGoogle Scholar

Bridger, A.F.C., and Murphy, J.R. (1998), Mars’ surface pressure tides and their behavior during global dust storms, J. Geophys. Res., 103(E4), 8587, doi:10.1029/98JE00242.Google Scholar

Briggs, G.A., and Leovy, C.B. (1974), Mariner observations of the Mars north polar hood, Bull. Am. Meteorol. Soc., 55(4), doi:10.1175/1520-0477(1974)055<0278:MOOTMN>2.0.CO;2.Google Scholar

Cahoy, K.L., Hinson, D.P., and Tyler, G.L. (2007), Characterization of a semidiurnal eastward-propagating tide at high northern latitudes with Mars Global Surveyor electron density profiles, Geophys. Res. Lett., 34(15), L15201, doi:10.1029/2007GL030449.Google Scholar

Cavalié, T., Billebaud, F., Encrenaz, T., et al. (2008), Vertical temperature profile and mesospheric winds retrieval on Mars from CO millimeter observations, Astron. Astrophys., 489(2), 795–809, doi:10.1051/0004-6361:200809815.Google Scholar

Chapman, S., and Lindzen, R.S. (1970), Atmospheric Tides – Thermal and Gravitational, Reidel, Dordrecht.Google Scholar

Charney, J.G. (1947), The dynamics of long waves in a baroclinc westerly current, J. Meteorol., 4(5), 136–162, doi:10.1175/1520-0469(1947)004<0136:TDOLWI>2.0.CO;2.Google Scholar

Christensen, P.R. (1988), Global albedo variations on Mars: implications for active aeolian transport, deposition, and erosion, J. Geophys. Res., 93(B7), 7611, doi:10.1029/JB093iB07p07611.Google Scholar

Christensen, P.R., Bandfield, J.L., Hamilton, V.E., et al. (2001), Mars Global Surveyor Thermal Emission Spectrometer experiment: investigation description and surface science results, J. Geophys. Res., 106(E10), 23823, doi:10.1029/2000JE001370.Google Scholar

Christensen, P.R., Jakosky, B.M., Kieffer, H.H., et al. (2004), The Thermal Emission Imaging System (THEMIS) for the Mars 2001 Odyssey Mission, Space Sci. Rev., 110(1/2), 85–130, doi:10.1023/B:SPAC.0000021008.16305.94.Google Scholar

Clancy, R.T., Sandor, B.J., Moriarty-Schieven, G.H., and Smith, M.D. (2006), Mesospheric winds and temperatures from JCMT sub-millimeter CO line observations during the 2003 and 2005 Mars oppositions, Second Int. Work. Mars Atmos. Model. Obs., Granada, Spain, http://www-mars.lmd.jussieu.fr/granada2006/.Google Scholar

Colaprete, A., Haberle, R.M., and Toon, O.B. (2003), Formation of convective carbon dioxide clouds near the south pole of Mars, J. Geophys. Res., 108(E7), 5081, doi:10.1029/2003JE002053.Google Scholar

Colaprete, A., Barnes, J.R., Haberle, R.M., et al. (2005), Albedo of the south pole on Mars determined by topographic forcing of atmosphere dynamics, Nature, 435(7039), 184–188, doi:10.1038/nature03561.Google Scholar

Colaprete, A., Barnes, J.R., Haberle, R.M., and Montmessin, F. (2008), CO₂ clouds, CAPE and convection on Mars: observations and general circulation modeling, Planet. Space Sci., 56(2), 150–180, doi:10.1016/j.pss.2007.08.010.Google Scholar

Colburn, D.S., Pollack, J.B., and Haberle, R.M. (1988), Diurnal Variations in Optical Depth at Mars: Observations and Interpretations, NASA-TM-100057, A-88067, NAS 1.15:1000057.Google Scholar

Collins, M., Lewis, S.R., and Read, P.L. (1995), Regular and irregular baroclinic waves in a Martian general circulation model: a role for diurnal forcing?, Adv. Sp. Res., 16(6), 3–7, doi:10.1016/0273-1177(95)00243-8.CrossRefGoogle Scholar

Collins, M., Lewis, S.R., Read, P.L., and Hourdin, F. (1996), Baroclinic wave transitions in the Martian atmosphere, Icarus, 120(2), 344–357, doi:10.1006/icar.1996.0055.Google Scholar

Collins, M., Lewis, S.R., and Read, P.L. (1997), Gravity wave drag in a global circulation model of the Martian atmosphere: parameterisation and validation, Adv. Sp. Res., 19(8), 1245–1254, doi:10.1016/S0273-1177(97)00277-9.Google Scholar

Conrath, B.J. (1975), Thermal structure of the Martian atmosphere during the dissipation of the dust storm of 1971, Icarus, 24(1), 36–46, doi:10.1016/0019-1035(75)90156-6.Google Scholar

Conrath, B.J. (1976), Influence of planetary-scale topography on the diurnal thermal tide during the 1971 Martian dust storm, J. Atmos. Sci., 33, 2430–2439, doi:10.1175/1520-0469(1976)033<2430:IOPSTO>2.0.CO;2.Google Scholar

Conrath, B.J. (1981), Planetary-scale wave structure in the Martian atmosphere, Icarus, 48(2), 246–255, doi:10.1016/0019-1035(81)90107-X.Google Scholar

Conrath, B.J., Pearl, J.C., Smith, M.D., et al. (2000), Mars Global Surveyor Thermal Emission Spectrometer (TES) observations: atmospheric temperatures during aerobraking and science phasing, J. Geophys. Res., 105(E4), 9509, doi:10.1029/1999JE001095.Google Scholar

Creasey, J.E., Forbes, J.M., and Hinson, D.P. (2006), Global and seasonal distribution of gravity wave activity in Mars’ lower atmosphere derived from MGS radio occultation data, Geophys. Res. Lett., 33(1), doi:10.1029/2005GL024037.Google Scholar

Crisp, D. (1990), Infrared radiative transfer in the dust-free Martian atmosphere, J. Geophys. Res., 95(B9), 14577, doi:10.1029/JB095iB09p14577.CrossRefGoogle Scholar

Eady, E.T. (1949), Long waves and cyclone waves, Tellus, 1, 33–52, doi:10.1111/j.2153-3490.1949.tb01265.x.Google Scholar

Eckermann, S.D., Ma, J., and Zhu, X. (2011), Scale-dependent infrared radiative damping rates on Mars and their role in the deposition of gravity-wave momentum flux, Icarus, 211(1), 429–442, doi:10.1016/j.icarus.2010.10.029.Google Scholar

Edmonds, R.M., Murphy, J., Schofield, J.T., and Heavens, N.G. (2014), Considerations on the Presence of Gravity Wave Activity During MCS Limb Staring Observations, Fifth Int. Work. Mars Atmos. Model. Obs., Oxford, UK, http://www-mars.lmd.jussieu.fr/oxford2014/.Google Scholar

Forbes, J.M. (2008), Troposphere–Thermosphere Coupling by Thermal Tides at Earth and Mars, AGU Spring Meeting Abstracts, 1, 1.Google Scholar

Forbes, J.M., and Hagan, M.E. (2000), Diurnal Kelvin wave in the atmosphere of Mars: towards an understanding of “stationary” density structures observed by the MGS accelerometer, Geophys. Res. Lett., 27(21), 3563–3566, doi:10.1029/2000GL011850.Google Scholar

Forbes, J.M., Bridger, A.F.C., Bougher, S.W., et al. (2002), Nonmigrating tides in the thermosphere of Mars, J. Geophys. Res., 107(E11), 5113, doi:10.1029/2001JE001582.Google Scholar

Forget, F., Hourdin, F., Fournier, R., et al. (1999), Improved general circulation models of the Martian atmosphere from the surface to above 80 km, J. Geophys. Res., 104(E10), 24155, doi:10.1029/1999JE001025.Google Scholar

Formisano, V., Grassi, D., Orfei, R., et al. (2004), The Planetary Fourier Spectrometer (PFS) for Mars Express, In Mars Express – The Scientific Payload, Ed. by Wilson, A., Sci. Coord. by A. Chicarro, ESA SP-1240, Noordwijk, Netherlands, ESA Publications Division, 71–94, http://sci.esa.int/mars-express/34885-esa-sp-1240-mars-express-the-scientific-payload/.Google Scholar

Gadian, A.M. (1978), The dynamics of and the heat transfer by baroclinic eddies and large-scale stationary topographically forced long waves in the Martian atmosphere, Icarus, 33(3), 454–465, doi:10.1016/0019-1035(78)90184-7.Google Scholar

Geissler, P.E. (2005), Three decades of Martian surface changes, J. Geophys. Res., 110(E2), E02001, doi:10.1029/2004JE002345.Google Scholar

Gierasch, P.J., and Goody, R. (1968), A study of the thermal and dynamical structure of the Martian lower atmosphere, Planet. Space Sci., 16(5), 615–646, doi:10.1016/0032-0633(68)90102-5.Google Scholar

Gill, A.E. (1980), Some simple solutions for heat-induced tropical circulation, Quart. J. Roy. Meteor. Soc., 106, 447–462, doi:10.1002/qj.49710644905.Google Scholar

Gómez-Elvira, J., Armiens, C., Castaner, L., et al. (2012), REMS: the environmental sensor suite for the Mars Science Laboratory Rover, Space Sci. Rev., 170(1–4), 583–640, doi:10.1007/s11214-012-9921-1.Google Scholar

Goody, R., and Belton, M.J.S. (1967), A discussion of Martian atmospheric dynamics, Planet. Space Sci., 15(2), 247–256, doi:10.1016/0032-0633(67)90193-6.Google Scholar

Greeley, R., Lancaster, N., Lee, S., and Thomas, P. (1992), Martian aeolian processes, sediments, and features, In Mars, Kieffer, H.H., Jakosky, B.M., Snyder, C.W., and Mathews, M.S., Eds., University of Arizona Press, 730–766.Google Scholar

Greeley, R., Skypeck, A., and Pollack, J.B. (1993), Martian aeolian features and deposits: comparisons with general circulation model results, J. Geophys. Res., 98(E2), 3183, doi:10.1029/92JE02580.Google Scholar

Greybush, S.J., Wilson, R.J., Hoffman, R.N., et al. (2012), Ensemble Kalman filter data assimilation of Thermal Emission Spectrometer temperature retrievals into a Mars GCM, J. Geophys. Res., 117(E11), E11008, doi:10.1029/2012JE004097.Google Scholar

Gunnlaugsson, H.P., Holstein-Rathlou, C., Merrison, J.P., et al. (2008), Telltale wind indicator for the Mars Phoenix Lander, J. Geophys. Res., 113, E00A04, doi:10.1029/2007JE003008.Google Scholar

Guzewich, S.D., Talaat, E.R., and Waugh, D.W. (2012), Observations of planetary waves and nonmigrating tides by the Mars Climate Sounder, J. Geophys. Res., 117(E3), E03010, doi:10.1029/2011JE003924.Google Scholar

Guzewich, S.D., Toigo, A.D., Richardson, M.I., et al. (2013), The impact of a realistic vertical dust distribution on the simulation of the Martian General Circulation, J. Geophys. Res. Planets, 118(5), 980–993, doi:10.1002/jgre.20084.Google Scholar

Haberle, R.M., and Catling, D.C. (1996), A Micro-Meteorological mission for global network science on Mars: rationale and measurement requirements, Planet. Space Sci., 44(11), 1361–1383, doi:10.1016/S0032-0633(96)00056-6.Google Scholar

Haberle, R.M., Leovy, C.B., and Pollack, J.B. (1982), Some effects of global dust storms on the atmospheric circulation of Mars, Icarus, 50(2–3), 322–367, doi:10.1016/0019-1035(82)90129-4.Google Scholar

Haberle, R.M., Houben, H.C., Hertenstein, R., and Herdtle, T. (1993a), A boundary-layer model for Mars: comparison with Viking Lander and entry data, J. Atmos. Sci., 50, 1544–1559, doi:10.1175/1520-0469(1993)050<1544:ABLMFM>2.0.CO;2.Google Scholar

Haberle, R.M., Pollack, J.B., Barnes, J.R., et al. (1993b), Mars atmospheric dynamics as simulated by the NASA Ames General Circulation Model: 1. The zonal-mean circulation, J. Geophys. Res., 98(E2), 3093, doi:10.1029/92JE02946.Google Scholar

Haberle, R.M., Houben, H.C., Barnes, J.R., and Young, R.E. (1997), A simplified three-dimensional model for Martian climate studies, J. Geophys. Res., 102(E4), 9051, doi:10.1029/97JE00383.Google Scholar

Haberle, R.M., Joshi, M.M., Murphy, J.R., et al. (1999), General circulation model simulations of the Mars Pathfinder atmospheric structure investigation/meteorology data, J. Geophys. Res., 104(E4), 8957, doi:10.1029/1998JE900040.Google Scholar

Haberle, R.M., Gomez-Elvira, J., de la Torre Juarez, M., et al. (2014), Preliminary interpretation of the REMS pressure data from the first 100 sols of the MSL mission, J. Geophys. Res. Planets, 119(3), 440–453, doi:10.1002/2013JE004488.CrossRefGoogle Scholar

Hamilton, K., and Garcia, R.R. (1986), Theory and observations of the short-period normal mode oscillations of the atmosphere, J. Geophys. Res., 91(D11), 11867, doi:10.1029/JD091iD11p11867.Google Scholar

Hanel, R., Conrath, B.J., Hovis, W., et al. (1972), Investigation of the Martian environment by infrared spectroscopy on Mariner 9, Icarus, 17(2), 423–442, doi:10.1016/0019-1035(72)90009-7.Google Scholar

Hartogh, P., Medvedev, A.S., Kuroda, T., et al. (2005), Description and climatology of a new general circulation model of the Martian atmosphere, J. Geophys. Res., 110(E11), E11008, doi:10.1029/2005JE002498.Google Scholar

Hartogh, P., Medvedev, A.S., and Jarchow, C. (2007), Middle atmosphere polar warmings on Mars: simulations and study on the validation with sub-millimeter observations, Planet. Space Sci., 55(9), 1103–1112, doi:10.1016/j.pss.2006.11.018.Google Scholar

Hayne, P.O., Paige, D.A., Heavens, N.G., and the Mars Climate Sounder Science Team (2014), The role of snowfall in forming the seasonal ice caps of Mars: models and constraints from the Mars Climate Sounder, Icarus, 231, 122–130, doi:10.1016/j.icarus.2013.10.020.Google Scholar

Hayward, R.K., Fenton, L.K., and Titus, T.N. (2014), Mars Global Digital Dune Database (MGD3): global dune distribution and wind pattern observations, Icarus, 230, 38–46, doi:10.1016/j.icarus.2013.04.011.Google Scholar

Heavens, N.G., Richardson, M.I., Lawson, W.G., et al. (2010), Convective instability in the Martian middle atmosphere, Icarus, 208(2), 574–589, doi:10.1016/j.icarus.2010.03.023.Google Scholar

Hébrard, E., Listowski, C., Coll, P., et al. (2012), An aerodynamic roughness length map derived from extended Martian rock abundance data, J. Geophys. Res. Planets, 117(E4), doi:10.1029/2011JE003942.Google Scholar

Held, I.M., and Hou, A.Y. (1980), Nonlinear axially symmetric circulations in a nearly inviscid atmosphere, J. Atmos. Sci., 37(3), 515–533, doi:10.1175/1520-0469(1980)037<0515:NASCIA>2.0.CO;2.Google Scholar

Held, I.M., Ting, M., and Wang, H. (2002), Northern winter stationary waves: theory and modeling, J. Climate, 15, 2125–2144, doi:10.1175/1520-0442(2002)015<2125:NWSWTA>2.0.CO;2.Google Scholar

Hess, S.L. (1950), Some aspects of the meteorology of Mars., J. Atmos. Sci., 7(1), doi:10.1175/1520-0469(1950)007<0001: SAOTMO>2.0.CO;2.Google Scholar

Hess, S.L., Henry, R.M., Leovy, C.B., Ryan, J.A., and Tillman, J.E. (1977), Meteorological results from the surface of Mars: Viking 1 and 2, J. Geophys. Res., 82(28), 4559–4574, doi:10.1029/JS082i028p04559.Google Scholar

Hinson, D.P. (2006), Radio occultation measurements of transient eddies in the northern hemisphere of Mars, J. Geophy. Res., 111, E05002, doi:10.1029/2005JE002612.Google Scholar

Hinson, D.P., and Wang, H. (2010), Further observations of regional dust storms and baroclinic eddies in the northern hemisphere of Mars, Icarus, 206, 290–305, doi:10.1016/j.icarus.2009.08.019.Google Scholar

Hinson, D.P., and Wilson, R.J. (2002), Transient eddies in the southern hemisphere of Mars, Geophys. Res. Lett., 29(7), 1154, doi:10.1029/2001GL014103.Google Scholar

Hinson, D.P., and Wilson, R.J. (2004), Temperature inversions, thermal tides, and water ice clouds in the Martian tropics, J. Geophys. Res., 109, E01002, doi:10.1029/2003JE002129.Google Scholar

Hinson, D.P., Simpson, R.A., Twicken, J.D., Tyler, G.L., and Flasar, F.M. (1999), Initial results from radio occultation measurements with Mars Global Surveyor, J. Geophys. Res., 104(E11), 26997–27012, doi:10.1029/1999JE001069.Google Scholar

Hinson, D.P., Tyler, G.L., Hollingsworth, J.L., and Wilson, R.J. (2001), Radio occultation measurements of forced atmospheric waves on Mars, J. Geophys. Res. Planets, 106(E1), 1463–1480, doi:10.1029/2000JE001291.Google Scholar

Hinson, D.P., Wilson, R.J., Smith, M.D., and Conrath, B.J. (2003), Stationary planetary waves in the atmosphere of Mars during southern winter, J. Geophys. Res., 108(E1), 5004, doi:10.1029/2002JE001949.Google Scholar

Hinson, D.P., Pätzold, M., Wilson, R.J., et al. (2008a), Radio occultation measurements and MGCM simulations of Kelvin waves on Mars, Icarus, 193(1), 125–138, doi:10.1016/j.icarus.2007.09.009.Google Scholar

Hinson, D.P., Pätzold, M., Tellmann, S., Häusler, B., and Tyler, G.L. (2008b), The depth of the convective boundary layer on Mars, Icarus, 198(1), 57–66, doi:10.1016/j.icarus.2008.07.003.Google Scholar

Hinson, D.P., Wang, H., and Smith, M.D. (2012), A multi-year survey of dynamics near the surface in the northern hemisphere of Mars: short-period baroclinic waves and dust storms, Icarus, 219(1), 307–320, doi:10.1016/j.icarus.2012.03.001.Google Scholar

Hoffman, M.J., Greybush, S.J., John Wilson, R.J., et al. (2010), An ensemble Kalman filter data assimilation system for the Martian atmosphere: implementation and simulation experiments, Icarus, 209(2), 470–481, doi:10.1016/j.icarus.2010.03.034.Google Scholar

Hollingsworth, J.L., and Barnes, J.R. (1996), Forced stationary planetary waves in Mars’s winter atmosphere., J. Atmos. Sci., 53, doi:10.1175/1520-0469(1996)053<0428:FSPWIM>2.0.CO;2.Google Scholar

Hollingsworth, J.L., and Kahre, M.A. (2010), Extratropical cyclones, frontal waves, and Mars dust: modeling and considerations, Geophys. Res. Lett., 37(22), doi:10.1029/2010GL044262.Google Scholar

Hollingsworth, J.L., Haberle, R.M., Barnes, J.R., et al. (1996), Orographic control of storm zones on Mars, Nature, 380(6573), 413–416, doi:10.1038/380413a0.Google Scholar

Hollingsworth, J.L., Haberle, R.M., and Schaeffer, J. (1997), Seasonal variations of storm zones on Mars, Adv. Sp. Res., 19(8), 1237–1240, doi:10.1016/S0273-1177(97)00275-5.Google Scholar

Hollingsworth, J.L., Kahre, M.A., Haberle, R.M., and Montmessin, F. (2011), Radiatively-active aerosols within Mars’ atmosphere: implications on the weather and climate as simulated by the NASA ARC Mars GCM, in Fourth Int. Work. Mars Atmos. Model. Obs., Paris, France, http://www-mars.lmd.jussieu.fr/paris2011/.Google Scholar

Holstein-Rathlou, C., Gunnlaugsson, H.P., Iversen, J.J., et al. (2014), Mars wind as seen by the NASA Phoenix Lander telltale, in Eighth Int. Conf. Mars, www.hou.usra.edu/meetings/8thmars2014/.Google Scholar

Holton, J.R., and Hakim, G.J. (2013), An Introduction to Dynamic Meteorology, Fifth Ed., Academic Press.Google Scholar

Holton, J.R., Haynes, P.H., McIntyre, M.E., et al. (1995), Stratosphere-troposphere exchange, Rev. Geophys., 33(4), 403, doi:10.1029/95RG02097.Google Scholar

Hourdin, F., Forget, F., and Talagrand, O. (1995), The sensitivity of the Martian surface pressure and atmospheric mass budget to various parameters: a comparison between numerical simulations and Viking observations, J. Geophys. Res., 100(E3), 5501, doi:10.1029/94JE03079.Google Scholar

Hu, R., Cahoy, K., and Zuber, M.T. (2012), Mars atmospheric CO₂ condensation above the north and south poles as revealed by radio occultation, climate sounder, and laser ranging observations, J. Geophys. Res., 117, E07002, doi:10.1029/2012JE004087.Google Scholar

Imamura, T., and Ogawa, T. (1995), Radiative damping of gravity waves in the terrestrial planetary atmospheres, Geophys. Res. Lett., 22(3), 267–270, doi:10.1029/94GL02998.Google Scholar

Joshi, M.M., Lewis, S.R., Read, P.L., and Catling, D.C. (1994), Western boundary currents in the atmosphere of Mars, Nature, 367(6463), 548–552, doi:10.1038/367548a0.Google Scholar

Joshi, M.M., Lawrence, B.N., and Lewis, S.R. (1995a), Gravity wave drag in three-dimensional atmospheric models of Mars, J. Geophys. Res., 100(E10), 21235, doi:10.1029/95JE02486.Google Scholar

Joshi, M.M., Lewis, S.R., Read, P.L., and Catling, D.C. (1995b), Western boundary currents in the Martian atmosphere: numerical simulations and observational evidence, J. Geophys. Res., 100(E3), 5485–5500, doi:10.1029/94JE02716.Google Scholar

Joshi, M.M., Haberle, R.M., Barnes, J.R., Murphy, J.R., and Schaeffer, J. (1997), Low-level jets in the NASA Ames Mars general circulation model, J. Geophys. Res., 102(E3), 6511, doi:10.1029/96JE03765.Google Scholar

Kahn, R. (1983), Some observational constraints on the global-scale wind systems of Mars, J. Geophys. Res., 88(A12), 10189, doi:10.1029/JA088iA12p10189.Google Scholar

Kahre, M.A., Haberle, R.M., Hollingsworth, J.L., and Wilson, R.J. (2014), Coupling the Mars dust and water cycles: investigating the role of clouds in controlling the vertical distribution of dust during N.H. summer, in Fifth Int. Work. Mars Atmos. Model. Obs., Oxford, UK, http://www-mars.lmd.jussieu.fr/oxford2014/.Google Scholar

Kavulich, M.J., Szunyogh, I., Gyarmati, G., and Wilson, R.J. (2013), Local dynamics of baroclinic waves in the Martian atmosphere, J. Atmos. Sci., 70, 3415–3447, doi:10.1175/JAS-D-12-0262.1.Google Scholar

Kieffer, H.H., Martin, T.Z., Peterfreund, A.R., et al. (1977), Thermal and albedo mapping of Mars during the Viking primary mission, J. Geophys. Res., 82(28), 4249–4291, doi:10.1029/JS082i028p04249.Google Scholar

Kleinböhl, A., Wilson, R.J., Kass, D., Schofield, J.T., and McCleese, D.J. (2013), The semidiurnal tide in the middle atmosphere of Mars, Geophys. Res. Lett., 40(10), 1952–1959, doi:10.1002/grl.50497.Google Scholar

Kondratyev, K.I., and Hunt, G.E. (1982), Weather and Climate on Planets, Pergamon Press.Google Scholar

Kuroda, T., Medvedev, A.S., Hartogh, P., and Takahashi, M. (2009), On forcing the winter polar warmings in the Martian middle atmosphere during dust storms, J. Met. Soc. Japan, 87(5), 913–921, doi:10.2151/jmsj.87.913.Google Scholar

Lahoz, W., Khattatov, B., and Menard, R., Eds. (2010), Data Assimilation – Making Sense of Observations, Springer.Google Scholar

Lait, L.R., and Stanford, J.L. (1988), Applications of Asynoptic Space–Time Fourier Transform Methods to Scanning Satellite Measurements, J. Atmos. Sci., 45(24), 3784–3799, doi:10.1175/1520-0469(1988)045<3784:AOASFT>2.0.CO;2.Google Scholar

Lee, C., Lawson, W.G., Richardson, M.I., et al. (2009), Thermal tides in the Martian middle atmosphere as seen by the Mars Climate Sounder, J. Geophys. Res., 114, E03005, doi:10.1029/2008JE003285.CrossRefGoogle ScholarPubMed

Lee, C., Lawson, W.G., Richardson, M.I., et al. (2011), Demonstration of ensemble data assimilation for Mars using DART, MarsWRF, and radiance observations from MGS TES, J. Geophys. Res., 116, E11011, doi:10.1029/2011JE003815.Google Scholar

Lellouch, E., Rosenqvist, J., Goldstein, J.J., Bougher, S.W., and Paubert, G. (1991), First absolute wind measurements in the middle atmosphere of Mars, Astrophys. J., 383, 401, doi:10.1086/170797.Google Scholar

Leovy, C.B. (1969), Mars: theoretical aspects of meteorology, Appl. Opt., 8(7), 1279–86, doi:10.1364/AO.8.001279.Google Scholar

Leovy, C.B. (1981), Observations of Martian tides over two annual cycles, J. Atmos. Sci., 38, 30–39, doi:10.1175/1520-0469(1981)038<0030:OOMTOT>2.0.CO;2.Google Scholar

Leovy, C.B., and Mintz, Y. (1969), Numerical simulation of the atmospheric circulation and climate of Mars, J. Atmos. Sci., 26(6), doi:10.1175/1520-0469(1969)026<1167:NSOTAC>2.0.CO;2.Google Scholar

Leovy, C.B., and Zurek, R.W. (1979), Thermal tides and Martian dust storms: direct evidence for coupling, J. Geophys. Res., 84(B6), 2956, doi:10.1029/JB084iB06p02956.Google Scholar

Leovy, C.B., Zurek, R.W., and Pollack, J.B. (1973), Mechanisms for Mars dust storms., J. Atmos. Sci., 30, doi:10.1175/1520-0469(1973)030<0749:MFMDS>2.0.CO;2.Google Scholar

Leovy, C.B., Tillman, J.E., Guest, W.R., and Barnes, J.R. (1985), Interannual variability of Martian weather, In Recent Advances in Planetary Meteorology, Cambridge Press, 69–84.Google Scholar

Lewis, S.R., and Barker, P.R. (2005), Atmospheric tides in a Mars general circulation model with data assimilation, Adv. Sp. Res., 36(11), 2162–2168, doi:10.1016/j.asr.2005.05.122.Google Scholar

Lewis, S.R., and Read, P.L. (1995), An operational data assimilation scheme for the Martian atmosphere, Adv. Sp. Res., 16(6), 9–13, doi:10.1016/0273-1177(95)00244-9.Google Scholar

Lewis, S.R., and Read, P.L. (2003), Equatorial jets in the dusty Martian atmosphere, J. Geophys. Res., 108, E4, 5034, doi:10.1029/2002JE001933.Google Scholar

Lewis, S.R., Collins, M., Read, P.L., et al. (1999), A climate database for Mars, J. Geophys. Res., 104(E10), 24177, doi:10.1029/1999JE001024.Google Scholar

Lewis, S.R., Read, P.L., Conrath, B.J., Pearl, J.C., and Smith, M.D. (2007), Assimilation of thermal emission spectrometer atmospheric data during the Mars Global Surveyor aerobraking period, Icarus, 192(2), 327–347, doi:10.1016/j.icarus.2007.08.009.Google Scholar

Lewis, S.R., Mulholland, D.P., Read, P.L., et al. (2016), The solsticial pause on Mars: 1. A planetary wave reanalysis, Icarus, 264, 456–464, doi:10.1016/j.icarus.2015.08.039.Google Scholar

Lian, Y., Richardson, M.I., Newman, C.E., et al. (2012), The Ashima/MIT Mars GCM and argon in the Martian atmosphere, Icarus, 218(2), 1043–1070, doi:10.1016/j.icarus.2012.02.012.Google Scholar

Lindzen, R.S., and Hou, A. (1988), Hadley circulations for zonally averaged heating centered off the equator, J. Atmos. Sci., 45(17), 2416–2427, doi:10.1175/1520-0469(1988)045<2416:HCFZAH>2.0.CO;2.Google Scholar

Liu, J., Richardson, M.I., and Wilson, R.J. (2003), An assessment of the global, seasonal, and interannual spacecraft record of Martian climate in the thermal infrared, J. Geophys. Res., 108, E8, 5089, doi:10.1029/2002JE001921.Google Scholar

Määttänen, A., Montmessin, F., Gondet, B., et al. (2010), Mapping the mesospheric CO₂ clouds on Mars: MEx/OMEGA and MEx/HRSC observations and challenges for atmospheric models, Icarus, 209(2), 452–469, doi:10.1016/j.icarus.2010.05.017.Google Scholar

Määttänen, A., Gondet, B., Montmessin, F., et al. (2014), Mesospheric CO₂ clouds on Mars: detection, properties and origin, Eighth Int. Conf. Mars., www.hou.usra.edu/meetings/8thmars2014/.Google Scholar

Madeleine, J.-B., Forget, F., Millour, E., Navarro, T., and Spiga, A. (2012), The influence of radiatively active water ice clouds on the Martian climate, Geophys. Res. Lett., 39(23), doi:10.1029/2012GL053564.Google Scholar

Magalhães, J.A. (1987), The Martian Hadley circulation: comparison of “viscous” model predictions to observations, Icarus, 70(3), 442–468, doi:10.1016/0019-1035(87)90087-X.Google Scholar

Magalhães, J.A., Schofield, J.T., and Seiff, A. (1999), Results of the Mars Pathfinder atmospheric structure investigation, J. Geophys. Res., 104(E4), 8943, doi:10.1029/1998JE900041.Google Scholar

Martin, T.Z. (1981), Mean thermal and albedo behavior of the Mars surface and atmosphere over a Martian year, Icarus, 45(2), 427–446, doi:10.1016/0019-1035(81)90045-2.Google Scholar

Martin, T.Z., and Kieffer, H.H. (1979), Thermal infrared properties of the Martian atmosphere: 2. The 15 µm band measurements, J. Geophys. Res., 84(B6), 2843, doi:10.1029/JB084iB06p02843.Google Scholar

McCleese, D.J., Schofield, J.T., Taylor, F.W., et al. (2008), Intense polar temperature inversion in the middle atmosphere on Mars, Nat. Geosci., 1(11), 745–749, doi:10.1038/ngeo332.Google Scholar

McCleese, D.J., Heavens, N.G., Schofield, J.T., et al. (2010), Structure and dynamics of the Martian lower and middle atmosphere as observed by the Mars Climate Sounder: seasonal variations in zonal mean temperature, dust, and water ice aerosols, J. Geophys. Res., 115, E12016, doi:10.1029/2010JE003677.Google Scholar

McConnochie, T.H., Bell, J.F. III, Savransky, D., et al. (2010), THEMIS-VIS observations of clouds in the Martian mesosphere: altitudes, wind speeds, and decameter-scale morphology, Icarus, 210(2), 545–565, doi:10.1016/j.icarus.2010.07.021.Google Scholar

McFarlane, N.A. (1987), The effect of orographically excited gravity wave drag on the general circulation of the lower stratosphere and troposphere, J. Atmos. Sci., 44, 1775–1800.Google Scholar

Medvedev, A.S., and Hartogh, P. (2007), Winter polar warmings and the meridional transport on Mars simulated with a general circulation model, Icarus, 186(1), 97–110, doi:10.1016/j.icarus.2006.08.020.Google Scholar

Medvedev, A.S., Yiğit, E., and Hartogh, P. (2011), Estimates of gravity wave drag on Mars: indication of a possible lower thermospheric wind reversal, Icarus, 211(1), 909–912, doi:10.1016/j.icarus.2010.10.013.Google Scholar

Mellon, M.T., Jakosky, B.M., Kieffer, H.H., and Christensen, P.R. (2000), High-resolution thermal inertia mapping from the Mars Global Surveyor Thermal Emission Spectrometer, Icarus, 148(2), 437–455, doi:10.1006/icar.2000.6503.Google Scholar

Mintz, Y. (1961), The general circulation of planetary atmospheres. In The Atmospheres of Mars and Venus, 107–146.Google Scholar

Mischna, M.A., Lee, C., and Richardson, M.I. (2012), Development of a fast, accurate radiative transfer model for the Martian atmosphere, past and present, J. Geophys. Res., 117(E10), E10009, doi:10.1029/2012JE004110.Google Scholar

Mitchell, D.M., Montabone, L., Thomson, S., and Read, P.L. (2015), Polar vortices on Earth and Mars: a comparative study of the climatology and variability from reanalyses, Quart. J. Roy. Met. Soc., 141(687), 550–562, doi:10.1002/qj.2376.Google Scholar

Miyoshi, Y., Forbes, J.M., and Moudden, Y. (2011), A new perspective on gravity waves in the Martian atmosphere: sources and features, J. Geophys. Res., 116(E9), E09009, doi:10.1029/2011JE003800.Google Scholar

Montabone, L., Lewis, S.R., Read, P.L., and Hinson, D.P. (2006), Validation of Martian meteorological data assimilation for MGS/TES using radio occultation measurements, Icarus, 185(1), 113–132, doi:10.1016/j.icarus.2006.07.012.Google Scholar

Montmessin, F., Forget, F., Rannou, P., Cabane, M., and Haberle, R.M. (2004), Origin and role of water ice clouds in the Martian water cycle as inferred from a general circulation model, J. Geophys. Res., 109(E10), E10004, doi:10.1029/2004JE002284.Google Scholar

Montmessin, F., Gondet, B., Bibring, J.-P., et al. (2007), Hyperspectral imaging of convective CO₂ ice clouds in the equatorial mesosphere of Mars, J. Geophys. Res., 112, E11590, doi:10.1029/2007JE002944.Google Scholar

Mooring, T.A., and Wilson, R.J. (2015), Transient eddies in the MACDA Mars reanalysis, J. Geophys. Res. Planets, 120, 1671–1696, doi:10.1002/2015JE004824.CrossRefGoogle Scholar

Moreno, R., Lellouch, E., Forget, F., et al. (2009), Wind measurements in Mars’ middle atmosphere: IRAM Plateau de Bure interferometric CO observations, Icarus, 201(2), 549–563, doi:10.1016/j.icarus.2009.01.027.Google Scholar

Moudden, Y., and Forbes, J.M. (2014), Insight into the seasonal asymmetry of nonmigrating tides on Mars, Geophys. Res. Lett., 41(7), 2631–2636, doi:10.1002/2014GL059535.Google Scholar

Moudden, Y., and McConnell, J.C. (2005), A new model for multiscale modeling of the Martian atmosphere, GM3, J. Geophys. Res., 110(E4), E04001, doi:10.1029/2004JE002354.Google Scholar

Moudden, Y., and Forbes, J.M. (2008a), Effects of vertically propagating thermal tides on the mean structure and dynamics of Mars’ lower thermosphere, Geophys. Res. Lett., 35, L23805, doi:10.1029/2008GL036086.Google Scholar

Moudden, Y., and Forbes, J.M. (2008b), Topographic connections with density waves in Mars’ aerobraking regime, J. Geophys. Res., 113, E11009, doi:10.1029/2008JE003107.CrossRefGoogle Scholar

Mulholland, D.P., Lewis, S.R., Read, P.L., Madaleine, J.-B., and Forget, F. (2016), The solsticial pause on Mars: 2. Modeling and investigation of causes, Icarus, 264, 465–477, doi:10.1016/j.icarus.2015.08.038.Google Scholar

Murphy, J.R., Leovy, C.B., and Tillman, J.E. (1990), Observations of Martian surface winds at the Viking Lander 1 Site, J. Geophys. Res., 95(B9), 14555, doi:10.1029/JB095iB09p14555.Google Scholar

Navarro, T., Forget, F., Millour, E., and Greybush, S.J. (2014), Detection of detached dust layers in the Martian atmosphere from their thermal signature using assimilation, Geophys. Res. Lett., 41, 6620–6626, doi:10.1002/1014GL061377.Google Scholar

Nayvelt, L., Gierasch, P.J., and Cook, K.H. (1997), Modeling and observations of Martian stationary waves, J. Atmos. Sci., 54, doi:10.1175/1520-0469(1997)054<0986:MAOOMS>2.0.CO;2.Google Scholar

Niver, D.S., and Hess, S.L. (1982), Band-pass filtering of one year of daily mean pressures on Mars, J. Geophys. Res., 87(B12), 10191, doi:10.1029/JB087iB12p10191.Google Scholar

Pätzold, M., Neubauer, F.M., Carone, L., et al. (2004), MaRS: Mars Express Orbiter Radio Science, In Mars Express – The Scientific Payload, Ed. by Wilson, A., Sci. Coord. by A. Chicarro, ESA SP-1240, Noordwijk, Netherlands, ESA Publications Division, 71–94, http://sci.esa.int/mars-express/34885-esa-sp-1240-mars-express-the-scientific-payload/.Google Scholar

Pedlosky, J. (1979), Geophysical Fluid Dynamics, Springer.Google Scholar

Peixoto, J.P., and Oort, A.H. (1992), Physics of Climate, American Institute of Physics.Google Scholar

Pirraglia, J.A., and Conrath, B.J. (1974), Martian tidal pressure and wind field obtained from the Mariner 9 infrared spectroscopy experiment., J. Atmos. Sci., 31, doi:10.1175/1520-0469(1974)031<0318:MTPAWF>2.0.CO;2.Google Scholar

Pleskot, L.K., and Miner, E.D. (1981), Time variability of Martian bolometric albedo, Icarus, 45(1), 179–201, doi:10.1016/0019-1035(81)90013-0.Google Scholar

Pollack, J.B., Colburn, D.S., Flasar, F.M., et al. (1979), Properties and effects of dust particles suspended in the Martian atmosphere, J. Geophys. Res., 84(B6), 2929, doi:10.1029/JB084iB06p02929.Google Scholar

Pollack, J.B., Leovy, C.B., Greiman, P.W., and Mintz, Y. (1981), A Martian general circulation experiment with large topography, J. Atmos. Sci., 38, 3–29, doi:10.1175/1520-0469(1981)038<0003: AMGCEW>2.0.CO;2.Google Scholar

Pollack, J.B., Haberle, R.M., Schaeffer, J., and Lee, H. (1990), Simulations of the general circulation of the Martian atmosphere: 1. Polar processes, J. Geophys. Res., 95(B2), 1447–1473, doi:10.1029/JB095iB02p01447.Google Scholar

Putzig, N., and Mellon, M.T. (2007), Apparent thermal inertia and the surface heterogeneity of Mars, Icarus, 191(1), 68–94, doi:10.1016/j.icarus.2007.05.013.Google Scholar

Read, P.L., and Lewis, S.R. (2004), The Martian Climate Revisited – Atmosphere and Environment of a Desert Planet, Springer.Google Scholar

Richardson, M.I., and Wilson, R.J. (2002), A topographically forced asymmetry in the Martian circulation and climate., Nature, 416(6878), 298–301, doi:10.1038/416298a.Google Scholar

Richardson, M.I., Toigo, A.D., and Newman, C.E. (2007), PlanetWRF: a general purpose, local to global numerical model for planetary atmospheric and climate dynamics, J. Geophys. Res., 112(E9), E09001, doi:10.1029/2006JE002825.Google Scholar

Rothman, L.S., Gordon, I.E., Babikov, Y., et al. (2013), The HITRAN2012 molecular spectroscopic database, J. Quant. Spectroscopy Rad. Transfer, 130, 4–50, doi:10.1016/j.jqsrt.2013.07.002.Google Scholar

Rucker, M.S. (2014), The effects of clouds on transient baroclinic eddies in a Mars general circulation model, Master’s Thesis, Oregon State University, Corvallis, Oregon.Google Scholar

Ryan, J.A., Henry, R.M., Hess, S.L., et al. (1978), Mars meteorology: three seasons at the surface, Geophys. Res. Lett., 5(8), 715–718, doi:10.1029/GL005i008p00715.Google Scholar

Salby, M.L. (1982a), Sampling theory for asynoptic satellite observations. Part I: Space-time spectra, resolution, and aliasing, J. Atmos. Sci., 39(11), 2577–2600, doi:10.1175/1520-0469(1982)039<2577:STFASO>2.0.CO;2.Google Scholar

Salby, M.L. (1982b), Sampling theory for asynoptic satellite observations. Part II: Fast Fourier Synoptic Mapping, J. Atmos. Sci., 39(11), 2601–2614, doi:10.1175/1520-0469(1982)039<2601:STFASO>2.0.CO;2.Google Scholar

Santee, M.L., and Crisp, D. (1993), Thermal structure and dust loading of the Martian atmosphere during late southern summer: Mariner 9 revisited, J. Geophys. Res., 98(E2), 3261, doi:10.1029/92JE01896.Google Scholar

Santee, M.L., and Crisp, D. (1995), Diagnostic calculations of the circulation in the Martian atmosphere, J. Geophys. Res., 100(E3), 5465, doi:10.1029/94JE03207.Google Scholar

Sato, T.M., Fujiwara, H., Takahashi, Y.O., et al. (2011), Tidal variations in the Martian lower atmosphere inferred from Mars Express Planetary Fourier Spectrometer temperature data, Geophys. Res. Lett., 38(24), doi:10.1029/2011GL050348.Google Scholar

Savijärvi, H. (1995), Mars boundary layer modeling: diurnal moisture cycle and soil properties at the Viking Lander 1 site, Icarus, 117(1), 120–127, doi:10.1006/icar.1995.1146.Google Scholar

Savijärvi, H., and Siili, T. (1993), The Martian slope winds and the nocturnal PBL jet, J. Atmos. Sci., 50, 77–88, doi:10.1175/1520-0469(1993)050<0077:TMSWAT>2.0.CO;2.Google Scholar

Savijärvi, H., Crisp, D., and Harri, A.-M. (2005), Effects of CO₂ and dust on present-day solar radiation and climate on Mars, Q. J. R. Meteorol. Soc., 131(611), 2907–2922, doi:10.1256/qj.04.09.Google Scholar

Schneider, E.K. (1983), Martian great dust storms: interpretive axially symmetric models, Icarus, 55(2), 302–331, doi:10.1016/0019-1035(83)90084-2.Google Scholar

Schofield, J.T., Barnes, J.R., Crisp, D., et al. (1997), The Mars Pathfinder atmospheric structure investigation/meteorology (ASI/MET) experiment., Science, 278(5344), 1752–1758, doi:10.1126/science.278.5344.1752.Google Scholar

Sharman, R.D., and Ryan, J.A. (1980), Mars atmosphere pressure periodicities from Viking observations, J. Atmos. Sci., 37, 1994–2001, doi:10.1175/1520-0469(1980)037<1994:MAPPFV>2.0.CO;2.Google Scholar

Shia, R.-L., Yung, Y.L., Allen, M., Zurek, R.W., and Crisp, D. (1989), Sensitivity study of advection and diffusion coefficients in a two-dimensional stratospheric model using excess carbon 14 data, J. Geophys. Res., 94(D15), 18467, doi:10.1029/JD094iD15p18467.Google Scholar

Smith, M.D. (2004), Interannual variability in TES atmospheric observations of Mars during 1999–2003, Icarus, 167(1), 148–165, doi:10.1016/j.icarus.2003.09.010.Google Scholar

Smith, M.D. (2008), Spacecraft observations of the Martian atmosphere, Ann. Rev. Earth Planet. Sci., 36(1), 191–219, doi:10.1146/annurev.earth.36.031207.124334.Google Scholar

Smith, M. D. (2009), THEMIS observations of Mars aerosol optical depth from 2002–2008, Icarus, 202(2), 444–452, doi:10.1016/j.icarus.2009.03.027.Google Scholar

Smith, M.D., Pearl, J.C., Conrath, B.J., and Christensen, P.R. (2001a), One Martian year of atmospheric observations by the thermal emission spectrometer, Geophys. Res. Lett., 28(22), 4263–4266, doi:10.1029/2001GL013608.Google Scholar

Smith, M.D., Pearl, J.C., Conrath, B.J., and Christensen, P.R. (2001b), Thermal Emission Spectrometer results: Mars atmospheric thermal structure and aerosol distribution, J. Geophys. Res., 106(E10), 23929, doi:10.1029/2000JE001321.Google Scholar

Smith, M.D., Conrath, B.J., Pearl, J.C., and Christensen, P.R. (2002), Thermal Emission Spectrometer observations of Martian planet-encircling dust storm 2001A, Icarus, 157(1), 259–263, doi:10.1006/icar.2001.6797.Google Scholar

Smith, M.D., Wolff, M.J., Spanovich, N., et al. (2006), One Martian year of atmospheric observations using MER Mini-TES, J. Geophys. Res., 111(E12), E12S13, doi:10.1029/2006JE002770.Google Scholar

Sonnabend, G., Sornig, M., Krötz, P.J., Schieder, R.T., and Fast, K.E. (2006), High spatial resolution mapping of Mars mesospheric zonal winds by infrared heterodyne spectroscopy of CO₂, Geophys. Res. Lett., 33(18), L18201, doi:10.1029/2006GL026900.Google Scholar

Sonnabend, G., Sornig, M., Kroetz, P., and Stupar, D. (2012), Mars mesospheric zonal wind around northern spring equinox from infrared heterodyne observations of CO₂, Icarus, 217(1), 315–321, doi:10.1016/j.icarus.2011.11.009.Google Scholar

Spiga, A., Forget, F., Lewis, S.R., and Hinson, D.P. (2010), Structure and dynamics of the convective boundary layer on Mars as inferred from large-eddy simulations and remote-sensing measurements, Q. J. R. Meteorol. Soc., 136(647), 414–428, doi:10.1002/qj.563.Google Scholar

Sprague, A.L., Boynton, W.V, Kerry, K.E., et al. (2004), Mars’ south polar Ar enhancement: a tracer for south polar seasonal meridional mixing, Science, 306(5700), 1364–7, doi:10.1126/science.1098496.Google Scholar

Sprague, A.L., Boynton, W.V., Kerry, K.E., et al. (2007), Mars’ atmospheric argon: tracer for understanding Martian atmospheric circulation and dynamics, J. Geophys. Res., 112(E3), E03S02, doi:10.1029/2005JE002597.Google Scholar

Sprague, A.L., Boynton, W.V., Forget, F., et al. (2012), Interannual similarity and variation in seasonal circulation of Mars’ atmospheric Ar as seen by the Gamma Ray Spectrometer on Mars Odyssey, J. Geophys. Res. Planets, 117(E4), doi:10.1029/2011JE003873.Google Scholar

Steele, L.J., Lewis, S.R., Patel, M.R., et al. (2014a), The seasonal cycle of water vapor on Mars from assimilation of Thermal Emission Spectrometer data, Icarus, 237, 97–115, doi:10.1016/j.icarus.2014.04.017.Google Scholar

Steele, L.J., Lewis, S.R., and Patel, M.R. (2014b), The radiative impact of water ice clouds from a reanalysis of Mars Climate Sounder data, Geophys. Res. Lett., 41, 4471–4478, doi:10.1002/2014GL060235.Google Scholar

Sullivan, R., Greeley, R., Kraft, M., et al. (2000), Results of the Imager for Mars Pathfinder windsock experiment, J. Geophys. Res., 105(E10), 24547, doi:10.1029/1999JE001234.Google Scholar

Sutton, J.L., Levoy, C.B., and Tillman, J.E. (1978), Diurnal variations of the Martian surface layer meteorological parameters during the first 45 sols at two Viking Lander sites, J. Atmos. Sci., 35, 2346–2355, doi:10.1175/1520-0469(1978)035<2346:DVOTMS>2.0.CO;2.Google Scholar

Szwast, M.A., Richardson, M.I., and Vasavada, A.R. (2006), Surface dust redistribution on Mars as observed by the Mars Global Surveyor and Viking Orbiters, J. Geoph. Res., 111(E11), E11008, doi:10.1029/2005JE002485.Google Scholar

Takahashi, Y.O., Fujiwara, H., Fukunishi, H., et al. (2003), Topographically induced north–south asymmetry of the meridional circulation in the Martian atmosphere, J. Geophys. Res., 108(E3), 5018, doi:10.1029/2001JE001638.Google Scholar

Takahashi, Y.O., Fujiwara, H., and Fukunishi, H. (2006), Vertical and latitudinal structure of the migrating diurnal tide in the Martian atmosphere: numerical investigations, J. Geophys. Res., 111(E1), E01003, doi:10.1029/2005JE002543.Google Scholar

Tellmann, S., Pätzold, M., Häusler, B., Hinson, D.P., and Tyler, G.L. (2013), The structure of Mars lower atmosphere from Mars Express Radio Science (MaRS) occultation measurements, J. Geophys. Res. Planets, 118(2), 306–320, doi:10.1002/jgre.20058.Google Scholar

Théodore, B., Lellouch, E., Chassefière, E., and Hauchecorne, A. (1993), Solstitial temperature inversions in the Martian middle atmosphere: observational clues and 2-D modeling, Icarus, 105(2), 512–528, doi:10.1006/icar.1993.1145.CrossRefGoogle Scholar

Thomas, P., Veverka, J., Lee, S., and Bloom, A. (1981), Classification of wind streaks on Mars, Icarus, 45(1), 124–153, doi:10.1016/0019-1035(81)90010-5.Google Scholar

Tillman, J.E. (1988), Mars global atmospheric oscillations: annually synchronized, transient normal-mode oscillations and the triggering of global dust storms, J. Geophys. Res., 93(D8), 9433, doi:10.1029/JD093iD08p09433.Google Scholar

Tillman, J.E., Henry, R.M., and Hess, S.L. (1979), Frontal systems during passage of the Martian north polar hood over the Viking Lander 2 site prior to the first 1977 dust storm, J. Geophys. Res., 84(B6), 2947, doi:10.1029/JB084iB06p02947.Google Scholar

Tillman, J.E., Johnson, N.C., Guttorp, P., and Percival, D.B. (1993), The Martian annual atmospheric pressure cycle: years without great dust storms, J. Geophys. Res., 98(E6), 10963, doi:10.1029/93JE01084.Google Scholar

Toigo, A.D., Richardson, M.I., Wilson, R.J., Wang, H., and Ingersoll, A.P. (2002), A first look at dust lifting and dust storms near the south pole of Mars with a mesoscale model, J. Geophys. Res., 107(E7), doi:10.1029/2011JE001592.Google Scholar

Tyler, D., and Barnes, J.R. (2005), A mesoscale model study of summertime atmospheric circulations in the north polar region of Mars, J. Geophys. Res., 110(E6), E06007, doi:10.1029/2004JE002356.Google Scholar

Tyler, D., and Barnes, J.R. (2013), Mesoscale modeling of the circulation in the Gale Crater region: an investigation into the complex forcing of convective boundary layer depths, Mars, 8, 58–77, doi:10.1555/mars.2013.0003.Google Scholar

Tyler, D., and Barnes, J.R. (2014), Atmospheric mesoscale modeling of water and clouds during northern summer on Mars, Icarus, 237, 388–414, doi:10.1016/j.icarus.2014.04.020.Google Scholar

Tyler, D., and Barnes, J.R. (2015), Convergent crater circulations on Mars: influence on the surface pressure cycle and the depth of the convective boundary layer, Geophys. Res. Lett., 42(18), 7343–7350, doi:10.1002/2015GL064957.Google Scholar

Wang, H. (2007), Dust storms originating in the northern hemisphere during the third mapping year of Mars Global Surveyor, Icarus, 189(2), 325–343, doi:10.1016/j.icarus.2007.01.014.Google Scholar

Wang, H., and Ingersoll, A.P. (2003), Cloud-tracked winds for the first Mars Global Surveyor mapping year, J. Geophys. Res., 108(E9), 5110, doi:10.1029/2003JE002107.Google Scholar

Wang, H., and Richardson, M.I. (2015), The origin, evolution, and trajectory of large dust storms on Mars during Mars Years 24–30 (1999–2011), Icarus, 251, 112–127, doi:10.1016/j.icarus.2013.10.033.Google Scholar

Wang, H., Richardson, M.I., Wilson, R.J., et al. (2003), Cyclones, tides, and the origin of a cross-equatorial dust storm on Mars, Geophys. Res. Lett., 30(9), 1488, doi:10.1029/2002GL016828.Google Scholar

Wang, H., Zurek, R.W., and Richardson, M.I. (2005), Relationship between frontal dust storms and transient eddy activity in the northern hemisphere of Mars as observed by Mars Global Surveyor, J. Geophys. Res., 110(E7), E07005, doi:10.1029/2005JE002423.Google Scholar

Wang, H., Toigo, A.D., and Richardson, M.I. (2011), Curvilinear features in the southern hemisphere observed by Mars Global Surveyor Mars Orbiter Camera, Icarus, 215(1), 242–252, doi:10.1016/j.icarus.2011.06.029.Google Scholar

Wang, H., Richardson, M.I., Toigo, A.D., and Newman, C.E. (2013), Zonal wavenumber three traveling waves in the northern hemisphere of Mars simulated with a general circulation model, Icarus, 223(2), 654–676, doi:10.1016/j.icarus.2013.01.004.Google Scholar

Webster, P.J. (1977), The low-latitude circulation of Mars, Icarus, 30(4), 626–649, doi:10.1016/0019-1035(77)90086-0.Google Scholar

Wilson, R.J. (1997), A general circulation model simulation of the Martian polar warming, Geophys. Res. Lett., 24(2), 123–126, doi:10.1029/96GL03814.Google Scholar

Wilson, R.J. (2000), Evidence for diurnal period Kelvin waves in the Martian atmosphere from Mars Global Surveyor TES data, Geophys. Res. Lett., 27(23), 3889–3892, doi:10.1029/2000GL012028.Google Scholar

Wilson, R.J. (2002), Evidence for nonmigrating thermal tides in the Mars upper atmosphere from the Mars Global Surveyor Accelerometer Experiment, Geophys. Res. Lett., 29(7), 1120, doi:10.1029/2001GL013975.Google Scholar

Wilson, R.J. (2011), Water ice clouds and thermal structure in the Martian tropics as revealed by Mars Climate Sounder, in Fourth Int. Workshop Mars Atmos. Model. Obs., Paris, France, http://www-mars.lmd.jussieu.fr/paris2011/.Google Scholar

Wilson, R.J. (2012a), The role of thermal tides in the Martian dust cycle, in Eur. Planet. Sci. Congr., Madrid, Spain, http://meetingorganizer.copernicus.org/EPSC2012/EPSC2012-798-1.pdf.Google Scholar

Wilson, R.J. (2012b), Thermal tides as revealed by Mars Climate Sounder, in Eur. Planet. Sci. Congr., Madrid, Spain, http://meetingorganizer.copernicus.org/EPSC2012/EPSC2012-825-1.pdf.Google Scholar

Wilson, R.J. (2015), The impact of planetary-scale thermal forcing and small-scale topography on the diurnal cycle of Martian surface pressure, Abstract P22A-07, presented at 2015 Fall Meeting, AGU, San Francisco, CA, 14–18 December, http://abstractsearch.agu.org/meetings/2015/FM/P22A-07.html.Google Scholar

Wilson, R.J., and Guzewich, S.D. (2014), Influence of water ice clouds on nighttime tropical temperature structure as seen by the Mars Climate Sounder, Geophys. Res. Lett., 41(10), 3375–3381, doi:10.1002/2014GL060086.Google Scholar

Wilson, R.J., and Hamilton, K. (1996), Comprehensive model simulation of thermal tides in the Martian atmosphere., J. Atmos. Sci., 53, doi:10.1175/1520-0469(1996)053<1290:CMSOTT>2.0.CO;2.Google Scholar

Wilson, R.J., and Richardson, M.I. (1999), Comparison of Mars GCM dust storm simulations with Viking mission observations, Fifth Int. Conf. Mars, Pasadena, California, www.lpi.usra.edu/meetings/5thMars99/pdf/sessguid.pdf.Google Scholar

Wilson, R.J., and Richardson, M.I. (2000), The Martian atmosphere during the Viking mission. 1: Infrared measurements of atmospheric temperatures revisited, Icarus, 145(2), 555–579, doi:10.1006/icar.2000.6378.Google Scholar

Wilson, R. J., Banfield, D., Conrath, B.J., and Smith, M.D. (2002), Traveling waves in the northern hemisphere of Mars, Geophys. Res. Lett., 29(14), 1684, doi:10.1029/2002GL014866.Google Scholar

Wilson, R.J., Hinson, D.P., and Smith, M.D. (2006), GCM simulations of transient eddies and frontal systems in the Martian atmosphere, Second Int. Work. Mars Atmos. Model. Obs., Granada, Spain, http://www-mars.lmd.jussieu.fr/granada2006/.Google Scholar

Wilson, R.J., Lewis, S.R., and Montabone, L. (2007), Thermal tides in an assimilation of three years of Thermal Emission Spectrometer data from Mars Global Surveyor, Seventh Int. Conf. Mars, Pasadena, California, www.lpi.usra.edu/meetings/7thmars2007/.Google Scholar

Wilson, R.J., Haberle, R.M., Noble, J., et al. (2008a), Simulation of the 2001 planet-encircling dust storm with the NASA/NOAA Mars general circulation model, Third Int. Work. Mars Atmos. Model. Obs., Williamsburg, Virginia, www.lpi.usra.edu/meetings/modeling2008/.Google Scholar

Wilson, R.J., Lewis, S.R., Montabone, L., and Smith, M.D. (2008b), Influence of water ice clouds on Martian tropical atmospheric temperatures, Geophys. Res. Lett., 35(7), doi:10.1029/2007GL032405.Google Scholar

Wilson, R.J., Millour, E., Navarro, T., Forget, F., and Kahre, M. (2014a), GCM simulations of aphelion season tropical cloud and temperature structure, Fifth Int. Work. Mars Atmos. Model. Obs., Oxford, UK, http://www-mars.lmd.jussieu.fr/oxford2014/.Google Scholar

Wilson, R.J., Guzewich, S.D., and Kleinböhl, A. (2014b), New progress and insights on thermal tides and their forcing from MCS and modeling, Eighth Int. Conf. Mars, Pasadena, California, www.hou.usra.edu/meetings/8thmars2014/.Google Scholar

Withers, P., Bougher, S.W., and Keating, G.J. (2003), The effects of topographically-controlled thermal tides in the Martian upper atmosphere as seen by the MGS accelerometer, Icarus, 164(1), 14–32, doi:10.1016/S0019-1035(03)00135-0.Google Scholar

Withers, P., Pratt, R., Bertaux, J.-L., and Montmessin, F. (2011), Observations of thermal tides in the middle atmosphere of Mars by the SPICAM instrument, J. Geophys. Res., 116(E11), E11005, doi:10.1029/2011JE003847.Google Scholar

Wolkenberg, P.M., and Wilson, R.J. (2014), Mars Climate Sounder observations of wave structure in the north polar middle atmosphere of Mars during the summer season, Eighth Int. Conf. Mars, Pasadena, California, www.hou.usra.edu/meetings/8thmars2014/.Google Scholar

Zalucha, A.M., Plumb, R.A., and Wilson, R.J. (2010), An analysis of the effect of topography on the Martian Hadley cells, J. Atmos. Sci., 67(3), 673–693, doi:10.1175/2009JAS3130.1.Google Scholar

Zhang, K.Q., Ingersoll, A.P., Kass, D.M., et al. (2001), Assimilation of Mars Global Surveyor atmospheric temperature data into a general circulation model, J. Geophys. Res., 106(E12), 32863, doi:10.1029/2000JE001330.Google Scholar

Zurek, R.W. (1976), Diurnal tide in the Martian atmosphere, J. Atmos. Sci., 33, 321–337, doi:10.1175/1520-0469(1976)033<0321:DTITMA>2.0.CO;2.Google Scholar

Zurek, R.W. (1981), Inference of dust opacities for the 1977 Martian great dust storms from Viking Lander 1 pressure data, Icarus, 45(1), 202–215, doi:10.1016/0019-1035(81)90014-2.Google Scholar

Zurek, R.W. (1986), Atmospheric tidal forcing of the zonal-mean circulation: the Martian dusty atmosphere, J. Atmos. Sci., 43, 652–670, doi:10.1175/1520-0469(1986)043<0652:ATFOTZ>2.0.CO;2.Google Scholar

Zurek, R.W. (1988), Free and forced modes in the Martian atmosphere, J. Geophys. Res., 93(D8), 9452, doi:10.1029/JD093iD08p09452.Google Scholar

Zurek, R.W., and Haberle, R.M. (1988), Zonally symmetric response to atmospheric tidal forcing in the dusty Martian atmosphere, J. Atmos. Sci., 45, 2469–2485, doi:10.1175/1520-0469(1988)045<2469:ZSRTAT>2.0.CO;2.Google Scholar

Zurek, R.W., and Leovy, C.B. (1981), Thermal tides in the dusty Martian atmosphere: a verification of theory, Science, 213(4506), 437–439, doi:10.1126/science.213.4506.437.Google Scholar

Zurek, R.W., Barnes, J.R., Haberle, R.M., et al. (1992), Dynamics of the atmosphere of Mars, In Mars, Kieffer, H.H., Jakosky, B.M., Snyder, C.W., and Mathews, M.S., Eds., University of Arizona Press, 835–933.Google Scholar