First direct measurements of enthalpy flux in the hurricane boundary layer: The CBLAST results
By Jun A. Zhang, P. Black, J. French, W. Drennan. 2008
175 citations recorded by the source corpus.
Subfields: Atmospheric Science, Oceanography
View Paper: https://www.semanticscholar.org/paper/deb99bbc2e576ef9641ad08d62fb3f218d59896a
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
- M. Montgomery
- Roger K. Smith
- G. Thomsen
- George H. Bryan
- Leo H. Holthuijsen
- Julie D. Pietrzak
- Mark D. Powell
- R. Houze
In Oceanography
- M. Montgomery
- Roger K. Smith
- G. Thomsen
- George H. Bryan
- Leo H. Holthuijsen
- Julie D. Pietrzak
- Mark D. Powell
- D. Nolan
Citations in the corpus
- Directional Wind-Wave Coupling in Fully Coupled Atmosphere-Wave-Ocean Models: Results from CBLAST-Hurricane (2013, result): “…the CBLAST-Hurricane also support these laboratory results, indicating that C K / C D is at about 0.4–0.7, less than that predicted by Emanuel (1995), for intensifying storms such as in Hurricane Fabian (2003) (a major category 4 hurricane) reported by Drennan et al. (2007) and Zhang et al. (2008).”
- Effects of Surface Exchange Coefficients and Turbulence Length Scales on the Intensity and Structure of Numerically Simulated Hurricanes (2012, background): “Several recent articles (e.g., Black et al. 2007; Zhang et al. 2008; Haus et al. 2010; Montgomery et al. 2010; Andreas 2011) have evaluated the conclusion from E95 that Ck/Cd is likely ;0.75 for intense TCs in nature because, according to E95, ‘‘. . .otherwise, the [modeled] wind speeds would be…”
- Wind and waves in extreme hurricanes (2012, background): “While our results extend the denominator of that ratio to more extreme wind speeds, Ce is still unknown at wind speeds above 29 m/s in the field [Drennan et al., 2007; Zhang et al., 2008] and 38 m/s in the laboratory [Haus et al., 2010].”
- Air-Sea Enthalpy and Momentum Exchange at Major Hurricane Wind Speeds Observed during CBLAST (2012, unknown): “Several potential errors were identified by sensitivity analyses using simulated data and the errors were optimally mitigated to reduce the uncertainty of the estimates.”
- Sensitivity of tropical‐cyclone models to the surface drag coefficient in different boundary‐layer schemes (2014, background): “…the surface drag and heat and moisture exchange coefficients are modified to fit the results of the Coupled Boundary Layer Air–Sea Transfer experiment (CBLAST; Black et al., 2007; Drennan et al., 2007; French et al., 2007; Zhang et al., 2008) to facilitate a proper comparison of the schemes.”