ER-2 Doppler Radar Investigations of the Eyewall of Hurricane Bonnie during the Convection and Moisture Experiment-3

By Gerald M. Heymsfield, J. Halverson, J. Simpson, Lin Tian, T. Bui. 2001

145 citations recorded by the source corpus.

Subfields: Atmospheric Science, Oceanography

View Paper: https://www.semanticscholar.org/paper/09a4ffb798560f9b8544c59b1cd96d1663713411

How researchers see this paper

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

In Atmospheric Science

1. M. Montgomery
2. Roger K. Smith
3. R. Houze
4. Nguyen Van Sang
5. R. Rogers
6. Jun A. Zhang
7. P. Reasor
8. J. Molinari

In Oceanography

1. M. Montgomery
2. Roger K. Smith
3. R. Houze
4. R. Rogers
5. Jun A. Zhang
6. P. Reasor
7. Nguyen Van Sang
8. Michael M. Bell

Citations in the corpus

• Tropical‐cyclone intensification and predictability in three dimensions (2008, methodology): “…lidar data and high-resolution numerical models (Simpson et al., 1998; Copyright 2008 Royal Meteorological Society Montgomery and Enagonio, 1998; Möller and Montgomery, 2000; Enagonio and Montgomery, 2001; Heymsfield et al., 2001; Braun, 2002; Hendricks et al., 2004; Montgomery et al., 2006a).”
• Convective-Scale Structure and Evolution during a High-Resolution Simulation of Tropical Cyclone Rapid Intensification (2010, background): “This evolution of the downdraft mass flux and temperature anomaly in the eye suggests the Shapiro and Willoughby (1982) and Heymsfield et al. (2001) mechanism may be operating here.”
• Multiscale Structure and Evolution of Hurricane Earl (2010) during Rapid Intensification (2015, background): “The exact role that CBs play has been tied to warming from upper-level subsidence around the periphery of the bursts (Chen and Zhang 2013; Zhang and Chen 2012; Guimond et al. 2010; Heymsfield et al. 2001) and to the stretching and subsequent axisymmetrization of low-level vorticity collocated with t”
• Recent Developments in the Fluid Dynamics of Tropical Cyclones (2017, unknown): “Heymsfield et al. 2001). The deep convection is maintained by appreciable moisture fluxes at the ocean-air interface, which sustain a conditionallyunstable thermodynamic environment. In a recent review paper, Montgomery and Smith (2014) examined and compared the four main paradigms that have been pr”
• Importance of the upper‐level warm core in the rapid intensification of a tropical cyclone (2012, background): “Many observational studies show that CBs either preceded RI or coincided with the onset of RI [e.g., Molinari et al., 1994, 1999; Reasor et al., 2009; Heymsfield et al., 2001; Fierro and Reisner, 2011].”
• Convective Contribution to the Genesis of Hurricane Ophelia (2005) (2009, background): “Two types of hypotheses have been 1 The term ‘‘hot tower’’ has also been used to describe tall, vertical, buoyant, rotating elements that are sometimes embedded in the eyewall of a fully developed hurricane (e.g., Heymsfield et al. 2001).”
• Rapid Intensification of a Sheared Tropical Storm (2010, background): “One common behavior in sheared tropical cyclones is the growth of cells downshear in the storm core and their subsequent dissipation upshear (Heymsfield et al. 2001; Black et al. 2002).”