Articles | Volume 16, issue 13
Atmos. Chem. Phys., 16, 8511–8519, 2016
https://doi.org/10.5194/acp-16-8511-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Atmos. Chem. Phys., 16, 8511–8519, 2016
https://doi.org/10.5194/acp-16-8511-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article 13 Jul 2016
Research article | 13 Jul 2016
Why did the storm ex-Gaston (2010) fail to redevelop during the PREDICT experiment?
Thomas M. Freismuth et al.
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Cited
9 citations as recorded by crossref.
- Remote Thermodynamic Impact of the Kuroshio Current on a Developing Tropical Cyclone Over the Western North Pacific in Boreal Fall K. Fujiwara et al. 10.1029/2019JD031356
- Observations and Predictability of a Nondeveloping Tropical Disturbance over the Eastern Atlantic A. Brammer et al. 10.1175/MWR-D-18-0065.1
- Impact of Mid- and Upper-Level Dry Air on Tropical Cyclone Genesis and Intensification: A Modeling Study of Durian (2001) Y. Wang et al. 10.1007/s00376-018-8039-0
- Finite-time circulation changes from topological rearrangement of distinguished curves and non-advective fluxes B. Rutherford & T. Dunkerton 10.1016/j.tcrr.2019.05.001
- Recent advances in research on tropical cyclogenesis B. Tang et al. 10.1016/j.tcrr.2020.04.004
- Dynamics of Lower-Tropospheric Vorticity in Idealized Simulations of Tropical Cyclone Formation Y. Wang et al. 10.1175/JAS-D-18-0219.1
- Dynamical properties of developing tropical cyclones using Lagrangian flow topology B. Rutherford et al. 10.1002/qj.3196
- Mesoscale Processes during the Genesis of Hurricane Karl (2010) M. Bell & M. Montgomery 10.1175/JAS-D-18-0161.1
- Size and Structure of Dry and Moist Reversible Tropical Cyclones D. Wang & Y. Lin 10.1175/JAS-D-19-0229.1
9 citations as recorded by crossref.
- Remote Thermodynamic Impact of the Kuroshio Current on a Developing Tropical Cyclone Over the Western North Pacific in Boreal Fall K. Fujiwara et al. 10.1029/2019JD031356
- Observations and Predictability of a Nondeveloping Tropical Disturbance over the Eastern Atlantic A. Brammer et al. 10.1175/MWR-D-18-0065.1
- Impact of Mid- and Upper-Level Dry Air on Tropical Cyclone Genesis and Intensification: A Modeling Study of Durian (2001) Y. Wang et al. 10.1007/s00376-018-8039-0
- Finite-time circulation changes from topological rearrangement of distinguished curves and non-advective fluxes B. Rutherford & T. Dunkerton 10.1016/j.tcrr.2019.05.001
- Recent advances in research on tropical cyclogenesis B. Tang et al. 10.1016/j.tcrr.2020.04.004
- Dynamics of Lower-Tropospheric Vorticity in Idealized Simulations of Tropical Cyclone Formation Y. Wang et al. 10.1175/JAS-D-18-0219.1
- Dynamical properties of developing tropical cyclones using Lagrangian flow topology B. Rutherford et al. 10.1002/qj.3196
- Mesoscale Processes during the Genesis of Hurricane Karl (2010) M. Bell & M. Montgomery 10.1175/JAS-D-18-0161.1
- Size and Structure of Dry and Moist Reversible Tropical Cyclones D. Wang & Y. Lin 10.1175/JAS-D-19-0229.1
Latest update: 17 Oct 2021
Short summary
Numerical model analyses are used to investigate the role of dry, environmental air in the failed redevelopment of a tropical cyclone (ex-Gaston, 2010). As early as 12:00 UTC 2 September 2010, a dry layer at and above 600 hPa results in a decrease in the vertical mass flux and vertical, relative vorticity. The intrusion of dry air led to a reduction in vorticity and a compromised pouch at these middle levels. This study supports work looking at the role of dry air in moist convection.
Numerical model analyses are used to investigate the role of dry, environmental air in the...
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