A study of a self-generated stratospheric sudden warming and its mesospheric-lower thermospheric impacts using the coupled TIME-GCM/CCM3

By Han-Li Liu, R. Roble. 2002

416 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Atmospheric Science

View Paper: https://www.semanticscholar.org/paper/f27d98b831f78fa015417daa8f14607ca0a62f65

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. Han-Li Liu
2. Jeff Forbes
3. L. P. Goncharenko
4. B. Fejer
5. Jorge L. Chau
6. N. Pedatella
7. J. Oberheide
8. R. Roble

In Atmospheric Science

1. Han-Li Liu
2. L. P. Goncharenko
3. Jorge L. Chau
4. B. Fejer
5. Jeff Forbes
6. Liying Qian
7. S. Solomon
8. R. Garcia

Citations in the corpus

• Evidence for stratosphere sudden warming‐ionosphere coupling due to vertically propagating tides (2010, background): “[3] It is well known that vertically propagating waves from the lower‐atmosphere can induce significant day‐to‐ day and week‐to‐week variability in the ionosphere [Forbes et al., 2000; Lastovicka, 2006 ].”
• Thermosphere extension of the Whole Atmosphere Community Climate Model (2010, background): “During the SSW, the large stratospheric wind change alters the gravity waves that propagate into the upper atmosphere, which in turn leads to changes in the MLT [Myrabø et al., 1984; Walterscheid et al., 2000; Liu and Roble, 2002; Coy et al., 2005; Ren et al., 2008].”
• A basis for efficient representation of the S-transform (2007, background): “The utility of S-transform analysis of a time series has been demonstrated in a range of geophysical fields such as: (i) analyzing internal atmospheric wave packets [20,21], (ii) atmospheric studies [22–26], (iii) characterization of seismic signals [27–30], (iv) global sea surface temperature analy”
• Sudden Stratospheric Warmings (2020, methodology): “This includes high lat-827 itude cooling, as well as a reversal of the zonal mean zonal winds from westward to east-828 ward (the opposite as in the stratosphere) (Labitzke, 1982; H.-L. Liu & Roble, 2002; Hoff-829 mann et al., 2007; Siskind et al., 2010; Limpasuvan et al., 2016).”
• The evolution of the stratopause during the 2006 major warming: Satellite data and assimilated meteorological analyses (2008, methodology): “PV is calculated from ECMWF winds and temperatures as described by Manney et al. [1996]. [16] Both GEOS-5 and ECMWF are operational systems, and they include very nearly the same data inputs.”
• Mesosphere inversion layers and stratosphere temperature enhancements (2004, background): “Thus the initial effects of a Northern Annular Mode signature are believed to appear at higher altitudes even though wave amplitudes may be less because of attenuation by the strong lower stratospheric eastward winds [Liu and Roble, 2002].”
• Ionospheric signatures of sudden stratospheric warming: Ion temperature at middle latitude (2008, methodology): “Our observations of this warming at 120–140 km agrees well with TIMEGCM predictions (see Figure 3 in Liu and Roble [2002] ), albeit it is observed at the middle latitude site.”