Surface Observations in the Hurricane Environment
By J. Cione, P. Black, S. Houston. 2000
142 citations recorded by the source corpus.
Subfields: Atmospheric Science, Oceanography
View Paper: https://www.semanticscholar.org/paper/16edfa0f7b01469438bfb4fea6ef7b7d8aa17725
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In Atmospheric Science
- M. Montgomery
- George H. Bryan
- Yuqing Wang
- Roger K. Smith
- J. Kepert
- R. edwards
- Richard L. Thompson
- Lon Curtis
In Oceanography
Citations in the corpus
- Convective Modes for Significant Severe Thunderstorms in the Contiguous United States. Part III: Tropical Cyclone Tornadoes (2012, background): “Furthermore, from an analysis of buoy data, Cione et al. (2000) showed thermal deficits accompanying vigorous convective bands, as well as a decrease in air–sea thermal deficit inwardwith respect to the dense precipitation of the inner region of hurricanes.”
- Effects of Surface Exchange Coefficients and Turbulence Length Scales on the Intensity and Structure of Numerically Simulated Hurricanes (2012, result): “…setup B, the sea surface temperature is 298C, which is chosen because it gives an initial air–sea temperature difference DT of 2.28C; this value of DT is similar to that of the RE87 setup (Table 1), and is near the climatological average value for hurricane environments (e.g., Cione et al. 2000).”
- Hurricane Maximum Intensity: Past and Present (2001, background): “Recent composite analysis of buoy and Coastal-Marine Automated Network data (Cione et al. 2000) similarly shows that relative humidity is not constant with radius.”
- The Dynamics of Boundary Layer Jets within the Tropical Cyclone Core. Part II: Nonlinear Enhancement (2001, methodology): “(1993), and Cione et al. (2000). We also analyze in detail the boundary layer flow beneath an inertially neutral storm, a case that is outside the validity range of the linear model.”
- The dynamics of boundary layer jets within the tropical cyclone core. Part I: Linear theory (2001, background): “The symmetric component is an extension of the symmetric vortex models of Rosenthal (1962) and Eliassen and Lystad (1977), while the asymmetric solution is believed to be new. It was shown that strong inwards advection of absolute angular momentum was necessary to produce the jet. In the linear mode”
- Midlevel Dry Intrusions as a Factor in Tornado Outbreaks Associated with Landfalling Tropical Cyclones from the Atlantic and Gulf of Mexico (2004, methodology): “As noted previously in section 2c, Cione et al. (2000) examined changes in air temperature and sea surface temperature changes in 37 hurricanes between 1975 and 1998, and concluded that the change in the spread between sea surface temperature and TA was primarily due to a reduction in TA (and not th”