On recent interannual variability of the Arctic winter mesosphere: Implications for tracer descent

By D. Siskind, Stephen D. Eckermann, L. Coy, J. McCormack, C. Randall. 2007

141 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/7af5d42a7de09e25da49d797300b122e141236fe

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Astronomy and Astrophysics

1. R. Akmaev
2. M. Ern
3. P. Preusse
4. Stephen D. Eckermann
5. M. Alexander
6. M. Mlynczak
7. J. Russell
8. Han-Li Liu

In Atmospheric Science

1. M. Ern
2. Stephen D. Eckermann
3. P. Preusse
4. R. Akmaev
5. M. Alexander
6. M. Mlynczak
7. J. Russell
8. Dong L. Wu

In Global and Planetary Change

1. Stephen D. Eckermann
2. A. Butler
3. F. Sassi
4. Gloria L. Manney
5. R. Garcia
6. S. Hardiman
7. T. Birner
8. M. Ern

Citations in the corpus

• Aura Microwave Limb Sounder observations of dynamics and transport during the record‐breaking 2009 Arctic stratospheric major warming (2009, background): “The stratopause broke down during the SSW, then reformed at very high altitude (near 75 km) [ Siskind et al. , 2007, M08].”
• WHOLE ATMOSPHERE MODELING: CONNECTING TERRESTRIAL AND SPACE WEATHER (2011, background): “…of climate and weather models to 115–250 km have also addressed long‐term changes in chemical composition including ionized species, related radiative and dynamical feedbacks, and short‐term variability [Fomichev et al., 2002; Sassi et al., 2004; Schmidt et al., 2006; Siskind et al., 2007].”
• Global Gravity Wave Variances from Aura MLS: Characteristics and Interpretation (2008, methodology): “However, analysis of SABER temperature data and global modeling by Siskind et al. (2007) suggests that the weakened 2006 vortex filtered out most orographic gravity waves, yielding a much-reduced upper-level orographic gravity wave drag relative to 2005, which then led to an anomalously strong…”
• Recent developments in gravity‐wave effects in climate models and the global distribution of gravity‐wave momentum flux from observations and models (2010, background): “The role of initial conditions in the troposphere and stratosphere provided by data assimilation in controlling a subsequent mesospheric forecast without a local dataassimilation constraint was similarly demonstrated in studies by Coy et al. (2005) and Siskind et al. (2007).”
• On the composite response of the MLT to major sudden stratospheric warming events with elevated stratopause (2016, background): “The downwelling fosters intrusion of MLT air into the stratosphere and impacts polar chemistry [Siskind et al., 2007;Manney et al., 2008; Kvissel et al., 2012].”
• Defining Sudden Stratospheric Warmings (2015, background): “…| Downloaded 04/28/21 03:38 AM UTC et al. 2012), equatorial tropospheric convective activity (e.g., Kodera 2006), polar tropospheric clouds (Kohma and Sato 2014), and mesospheric dynamics and the breakdown and reformation of the stratopause (e.g., Siskind et al. 2007; Manney et al. 2008).”
• Equatorial and Low Latitude Ionospheric Effects During Sudden Stratospheric Warming Events (2011, background): “Other effects include the extension of the polar vortex into the mesosphere and the displacement of the temperature peak associated with the stratopause up to 80 km (Siskind et al. 2007; Manney et al. 2009).”
• Geomagnetic activity and polar surface air temperature variability (2009, background): “, 2007], but stratospheric warmings can also be followed by large EPP effects due to enhanced mesospheric descent [Siskind et al., 2007].”
• Case studies of the mesospheric response to recent minor, major, and extended stratospheric warmings (2010, methodology): “shows that there was almost no planetary wave activity in the stratosphere after the 2006 SSW although, as noted previously [Siskind et al., 2007; Manney et al., 2008] there”
• The evolution of the stratopause during the 2006 major warming: Satellite data and assimilated meteorological analyses (2008, methodology): “…nonorographic GW scheme, since the temperature evolution described above (section 3.1) is consistent with a residual meridional circulation forced by GW drag producing enhanced descent over the pole that warms the stratopause region [e.g., Garcia and Boville, 1994; Siskind et al., 2007].”