Tropical Waves and the Quasi-Biennial Oscillation in a 7-km Global Climate Simulation

AbstractThis study investigates tropical waves and their role in driving a quasi-biennial oscillation (QBO)-like signal in stratospheric winds in a global 7-km-horizontal-resolution atmospheric general circulation model. The Nature Run (NR) is a 2-yr global mesoscale simulation of the Goddard Earth Observing System Model, version 5 (GEOS-5). In the tropics, there is evidence that the NR supports a broad range of convectively generated waves. The NR precipitation spectrum resembles the observed spectrum in many aspects, including the preference for westward-propagating waves. However, even with very high horizontal resolution and a healthy population of resolved waves, the zonal force provided by the resolved waves is still too low in the QBO region and parameterized gravity wave drag is the main driver of the NR QBO-like oscillation (NR-QBO). The authors suggest that causes include coarse vertical resolution and excessive dissipation. Nevertheless, the very-high-resolution NR provides an opportunity to an...

[1]  Maria Athanassiadou,et al.  Predictability of the quasi‐biennial oscillation and its northern winter teleconnection on seasonal to decadal timescales , 2014 .

[2]  Shian-Jiann Lin,et al.  Finite-volume transport on various cubed-sphere grids , 2007, J. Comput. Phys..

[3]  Matthew C. Wheeler,et al.  Convectively Coupled Equatorial Waves: Analysis of Clouds and Temperature in the Wavenumber–Frequency Domain , 1999 .

[4]  Shian‐Jiann Lin A “Vertically Lagrangian” Finite-Volume Dynamical Core for Global Models , 2004 .

[5]  D. Andrews,et al.  Planetary Waves in Horizontal and Vertical Shear: Asymptotic Theory for Equatorial Waves in Weak Shear , 1976 .

[6]  S. Hardiman,et al.  The Brewer–Dobson circulation inferred from ERA‐Interim , 2012 .

[7]  D. G. Andrews,et al.  Planetary Waves in Horizontal and Vertical Shear: The Generalized Eliassen-Palm Relation and the Mean Zonal Acceleration , 1976 .

[8]  Rolando R. Garcia,et al.  The excitation of equatorial waves by deep convection in the NCAR Community Climate Model (CCM3) , 2000 .

[9]  S. Watanabe,et al.  General aspects of a T213L256 middle atmosphere general circulation model , 2008 .

[10]  C. Frantzidis,et al.  Response to Reviewers Reviewer #1 , 2010 .

[11]  G. D. Nastrom,et al.  A Climatology of Atmospheric Wavenumber Spectra of Wind and Temperature Observed by Commercial Aircraft , 1985 .

[12]  Rolando R. Garcia,et al.  'Downward control' of the mean meridional circulation and temperature distribution of the polar winter stratosphere , 1994 .

[13]  Andrea Molod,et al.  Constraints on the Profiles of Total Water PDF in AGCMs from AIRS and a High-Resolution Model , 2012 .

[14]  R. Stolarski,et al.  Comparison of lower stratospheric tropical mean vertical velocities , 2008 .

[15]  E. Roeckner,et al.  Forcing of the quasi‐biennial oscillation from a broad spectrum of atmospheric waves , 2002 .

[16]  Julio T. Bacmeister,et al.  Rain Reevaporation, Boundary Layer Convection Interactions, and Pacific Rainfall Patterns in an AGCM , 2006 .

[17]  Adam A. Scaife,et al.  Realistic quasi‐biennial oscillations in a simulation of the global climate , 2000 .

[18]  T. Horinouchi,et al.  Wave–Mean Flow Interaction Associated with a QBO-like Oscillation Simulated in a Simplified GCM , 1998 .

[19]  J. Scinocca,et al.  Simulating the QBO in an Atmospheric General Circulation Model: Sensitivity to Resolved and Parameterized Forcing , 2016 .

[20]  G. Boer,et al.  QBO influence on extratropical predictive skill , 2008 .

[21]  Suzana J. Camargo,et al.  Revisiting the Influence of the Quasi-Biennial Oscillation on Tropical Cyclone Activity , 2010 .

[22]  Kevin Hamilton,et al.  Middle Atmosphere Simulated with High Vertical and Horizontal Resolution Versions of a GCM: Improvements in the Cold Pole Bias and Generation of a QBO-like Oscillation in the Tropics , 1999 .

[23]  J. Holton,et al.  A Theory of the Quasi-Biennial Oscillation , 1968 .

[24]  Bernard Legras,et al.  of Geophysical Research : Atmospheres Evaluating the advective Brewer-Dobson circulation in three reanalyses for the period 1979 – 2012 , 2015 .

[25]  Y. Hong,et al.  The TRMM Multisatellite Precipitation Analysis (TMPA): Quasi-Global, Multiyear, Combined-Sensor Precipitation Estimates at Fine Scales , 2007 .

[26]  M. Suárez,et al.  A proposal for the intercomparison of the dynamical cores of atmospheric general circulation models , 1994 .

[27]  T. Dunkerton,et al.  The Roles of Equatorial Trapped Waves and Internal Inertia–Gravity Waves in Driving the Quasi-Biennial Oscillation. Part I: Zonal Mean Wave Forcing , 2010 .

[28]  T. Dunkerton The role of gravity waves in the quasi‐biennial oscillation , 1997 .

[29]  J. Holton,et al.  An Updated Theory for the Quasi-Biennial Cycle of the Tropical Stratosphere , 1972 .

[30]  J. Bacmeister,et al.  On the simulation of the quasi‐biennial oscillation in the Community Atmosphere Model, version 5 , 2014 .

[31]  M. Giorgetta,et al.  The quasi-biennial oscillation in a warmer climate: sensitivity to different gravity wave parameterizations , 2015, Climate Dynamics.

[32]  T. Hinton,et al.  Stratospheric Variability in Twentieth-Century CMIP5 Simulations of the Met Office Climate Model: High Top versus Low Top , 2013 .

[33]  S. Schubert,et al.  MERRA: NASA’s Modern-Era Retrospective Analysis for Research and Applications , 2011 .

[34]  C. Jablonowski,et al.  Idealized Quasi-Biennial Oscillations in an Ensemble of Dry GCM Dynamical Cores , 2015 .

[35]  M. Alexander,et al.  Tropical Precipitation Variability and Convectively Coupled Equatorial Waves on Submonthly Time Scales in Reanalyses and TRMM , 2013 .

[36]  Lennart Bengtsson,et al.  Climatology and Forcing of the Quasi-Biennial Oscillation in the MAECHAM5 Model , 2006 .

[37]  S. Moorthi,et al.  Relaxed Arakawa-Schubert - A parameterization of moist convection for general circulation models , 1992 .

[38]  Norman A. McFarlane,et al.  The Effect of Orographically Excited Gravity Wave Drag on the General Circulation of the Lower Stratosphere and Troposphere , 1987 .

[39]  Tomoe Nasuno,et al.  A 20-Year Climatology of a NICAM AMIP-Type Simulation , 2015 .

[40]  Y. Kawatani,et al.  Weakened stratospheric quasibiennial oscillation driven by increased tropical mean upwelling , 2013, Nature.

[41]  M. Alexander,et al.  A convection‐based gravity wave parameterization in a general circulation model: Implementation and improvements on the QBO , 2014 .

[42]  John M. Wallace,et al.  Stratospheric Connection to Northern Hemisphere Wintertime Weather: Implications for Prediction , 2002 .

[43]  M. Alexander,et al.  Realistic simulations of atmospheric gravity waves over the continental U.S. using precipitation radar data , 2015 .

[44]  Karl E. Taylor,et al.  An overview of CMIP5 and the experiment design , 2012 .

[45]  J. Kiehl,et al.  Tracer transport by the diabatic circulation deduced from satellite observations , 1986 .

[46]  Toshitaka Tsuda,et al.  Global distribution of atmospheric waves in the equatorial upper troposphere and lower stratosphere: COSMIC observations of wave mean flow interactions , 2008 .

[47]  J. Holton Waves in the Equatorial Stratosphere Generated by Tropospheric Heat Sources , 1972 .

[48]  D. Ortland,et al.  Equatorial waves in High Resolution Dynamics Limb Sounder (HIRDLS) data , 2010 .

[49]  Kevin Hamilton,et al.  The quasi‐biennial oscillation , 2001 .

[50]  N. Butchart The Brewer‐Dobson circulation , 2014 .

[51]  R. Swinbank,et al.  Characteristics of stratospheric winds and temperatures produced by data assimilation , 1997 .

[52]  Masaaki Takahashi,et al.  Simulation of the stratospheric Quasi-Biennial Oscillation using a general circulation model , 1996 .