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Author Chassignet, E. ; Hurlburt, H. ; Metzger, E.J. ; Smedstad, O. ; Cummings, J. ; Halliwell, G. ; Bleck, R. ; Baraille, R. ; Wallcraft, A. ; Lozano, C. ; Tolman, H. ; Srinivasan, A. ; Hankin, S. ; Cornillon, P. ; Weisberg, R. ; Barth, A. ; He, R. ; Werner, F. ; Wilkin, J.
Title US GODAE: Global Ocean Prediction with the HYbrid Coordinate Ocean Model (HYCOM) Type $loc['typeJournal Article']
Year 2009 Publication Oceanography Abbreviated Journal Oceanog.
Volume 22
Issue 2
Pages 64-75
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Series Editor Series Title Abbreviated Series Title
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ISSN 1042-8275
ISBN Medium
Area Expedition Conference
Funding Approved $loc['no']
Call Number COAPS @ mfield @
Serial 390
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Author Cornillon, P. ; Adams, J. ; Blumenthal, M.B. ; Chassignet, E. ; Davis, E. ; Hankin, S. ; Kinter, J. ; Mendelssohn, R. ; Potemra, J. ; Srinivasan, A. ; Sirott, J.
Title NVODS and the Development of OPeNDAP Type $loc['typeJournal Article']
Year 2009 Publication Oceanography Abbreviated Journal Oceanog.
Volume 22
Issue 2
Pages 116-127
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Language Summary Language Original Title
Series Editor Series Title Abbreviated Series Title
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ISSN 1042-8275
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Funding Approved $loc['no']
Call Number COAPS @ mfield @
Serial 391
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Author Hurlburt, H. ; Brassington, G. ; Drillet, Y. ; Kamachi, M. ; Benkiran, M. ; Bourdallé-Badie, R. ; Chassignet, E. ; Jacobs, G. ; Galloudec, O. ; Lellouche, J.-M. ; Metzger, E.J. ; Oke, P. ; Pugh, T. ; Schiller, A. ; Smedstad, O. ; Tranchant, B. ; Tsujino, H. ; Usui, N. ; Wallcraft, A.
Title High-Resolution Global and Basin-Scale Ocean Analyses and Forecasts Type $loc['typeJournal Article']
Year 2009 Publication Oceanography Abbreviated Journal Oceanog.
Volume 22
Issue 3
Pages 110-127
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Series Editor Series Title Abbreviated Series Title
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ISSN 1042-8275
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Area Expedition Conference
Funding Approved $loc['no']
Call Number COAPS @ mfield @
Serial 675
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Author Dombrowsky, E. ; Bertino, L. ; Brassington, G. ; Chassignet, E. ; Davidson, F. ; Hurlburt, H. ; Kamachi, M. ; Lee, T. ; Martin, M. ; Mei, S. ; Tonani, M.
Title GODAE Systems in Operation Type $loc['typeJournal Article']
Year 2009 Publication Oceanography Abbreviated Journal Oceanog.
Volume 22
Issue 3
Pages 80-95
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Language Summary Language Original Title
Series Editor Series Title Abbreviated Series Title
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ISSN 1042-8275
ISBN Medium
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Funding Approved $loc['no']
Call Number COAPS @ mfield @
Serial 382
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Author Goni, G. ; DeMaria, M. ; Knaff, J. ; Sampson, C. ; Ginis, I. ; Bringas, F. ; Mavume, A. ; Lauer, C. ; Lin, I.I. ; Ali, M.M. ; Sandery, P. ; Ramos-Buarque, S. ; Kang, K.R. ; Mehra, A. ; Chassignet, E. ; Halliwell, G.
Title Applications of Satellite-Derived Ocean Measurements to Tropical Cyclone Intensity Forecasting Type $loc['typeJournal Article']
Year 2009 Publication Oceanography Abbreviated Journal Oceanog.
Volume 22
Issue 3
Pages 190-197
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Language Summary Language Original Title
Series Editor Series Title Abbreviated Series Title
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ISSN 1042-8275
ISBN Medium
Area Expedition Conference
Funding Approved $loc['no']
Call Number COAPS @ mfield @
Serial 384
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Author Cabrera, V.E., D. Solis, and D. Letson
Title Optimal crop insurance under climate variability: contrasting insurer and farmer interests Type $loc['typeJournal Article']
Year 2009 Publication Transactions of the ASABE Abbreviated Journal
Volume 52
Issue 2
Pages 623-631
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Funding Approved $loc['no']
Call Number COAPS @ mfield @
Serial 657
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Author Ahern, Kyle K.
Title Hurricane Boundary Layer Structure during Intensity Change: An Observational and Numerical Analysis Type $loc['typeManuscript']
Year 2019 Publication Florida State University College of Arts and Sciences Abbreviated Journal
Volume Issue Pages
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Call Number COAPS @ user @
Serial 1103
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Author Carstens, J
Title Tropical Cyclogenesis from Self-aggregated Convection in Numerical Simulations of Rotating Radiative-convective Equilibrium Type $loc['typeManuscript']
Year 2019 Publication Dissertations & Theses Abbreviated Journal Dissertations & Theses
Volume Issue Pages
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Abstract Organized convection is of critical importance in the tropical atmosphere. Recent advances in numerical modeling have revealed that moist convection can interact with its environment to transition from a quasi-random to organized state. This phenomenon, known as convective self-aggregation,is aided by feedbacks involving clouds, water vapor, and radiation that increase the spatial variance of column-integrated frozen moist static energy. Prior studies have shown self-aggregation to takeseveral different forms, including that of spontaneous tropical cyclogenesis in an environment of rotating radiative-convective equilibrium (RCE). This study expands upon previous work to address the processes leading to tropical cyclogenesis in this rotating RCE framework. More specifically,a three-dimensional, cloud-resolving numerical model is used to examine the self-aggregation of convection and potential cyclogenesis, and the background planetary vorticity is varied on an f-plane across simulations to represent a range of deep tropical and near-equatorial environments.Convection is initialized randomly in an otherwise homogeneous environment, with no background wind, precursor disturbance, or other synoptic-scale forcing.All simulations with planetary vorticity corresponding to latitudes from 10°to 20°generate intense tropical cyclones, with maximum wind speeds of 80 m s−1or above. Time to genesis varies widely, even within a five-member ensemble of 20°simulations, reflecting a potential degree of stochastic variability based in part on the initial random distribution of convection. Shared across this so-called “high-f” group is the emergence of a midlevel vortex in the days leading to genesis,which has dynamic and thermodynamic implications on its environment that facilitate the spinup of a low-level vortex. Tropical cyclogenesis is possible in this model even at values of Coriolis parameter as low as that representative of 1°. In these experiments, convection self-aggregates into a quasi-circular cluster, which then begins to rotate and gradually strengthen into a tropical storm, aided by near-surface inflow and shallow overturning radial circulations aloft within the aggregated cluster. Other experiments at these lower Coriolis parameters instead self-aggregate into an elongated band and fail to undergo cyclogenesis over the 100-day simulation. A large portion of this study is devoted to examining in greater detail the dynamic and thermodynamic evolution of cyclogenesis in these experiments and comparing the physical mechanisms to current theories.
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Publisher Florida State University - FCLA; ProQuest Dissertations & Theses Global
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Call Number COAPS @ user @
Serial 1054
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Author Buchanan, S. ; Misra, V. ; Bhardwaj, A.
Title https://rmets.onlinelibrary.wiley.com/doi/10.1002/joc.5450 Type $loc['typeJournal Article']
Year 2018 Publication International Journal of Climatology Abbreviated Journal
Volume 38
Issue 6
Pages 2651-2661
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Abstract The integrated kinetic energy (IKE) of a tropical cyclone (TC), a volume integration of the surface winds around the centre of the TC, is computed from a comprehensive surface wind (National Aeronautics and Space Administration’s (NASA) cross‐calibrated multi‐platform [CCMP]) analysis available over the global oceans to verify against IKE from wind radii estimates of extended best‐track data maintained by NOAA for the North Atlantic TCs. It is shown that CCMP surface wind analysis severely underestimates IKE largely from not resolving hurricane force winds for majority of the Atlantic TCs, under sampling short‐lived and small‐sized TCs. The seasonal cycle of the North Atlantic TC IKE also verifies poorly in the CCMP analysis. In this article we introduce proxy IKE (PIKE) based on the kinetic energy of the winds at the radius of the last closed isobar (ROCI), which shows promise for a wide range of TC sizes including the smaller‐sized TCs unresolved in the CCMP data set.
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Call Number COAPS @ mfield @
Serial 551
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Author Ali, M.M.
Title Is it high time to use ocean mean temperature for monsoon prediction? Type $loc['typeJournal Article']
Year 2020 Publication Atmosphera Abbreviated Journal Atmosphera
Volume Issue Pages
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Abstract A monsoon is a seasonal reversal in the prevailing wind direction, that is usually initiated by the land sea temperature contrast. The Indian summer monsoon, for example, is triggered when the land gets heated up more than the surrounding sea during the summer creating a pressure gradient between the land and the sea. It is well known that the ocean thermal energy required for fueling monsoon circulations comes from the upper layer of the ocean (e.g. Venugopal et al. 2018). But such amount of energy does not come from the top thin layer represented by sea surface temperature (SST) alone. Nevertheless, often SST does not represent the thermal energy available in the upper ocean, although this parameter has been the only oceanographic input to the cyclone and monsoon atmospheric numerical and statistical models.
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Serial 1116
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