Records
Links
Author
Izaurralde, R.C. ; Rosenberg, N.J. ; Brown, R.A. ; Legler, D.M. ; Tiscareño López, M. ; Srinivasan, R.
Title
Modeled effects of moderate and strong 'Los Niños' on crop productivity in North America
Type
$loc['typeJournal Article']
Year
1999
Publication
Agricultural and Forest Meteorology
Abbreviated Journal
Agricultural and Forest Meteorology
Volume
94
Issue
3-4
Pages
259-268
Keywords
El Nino ; El Nino Southern Oscillation (ENSO) ; EPIC ; corn ; wheat
Abstract
Address
Corporate Author
Thesis
Publisher
Place of Publication
Editor
Language
Summary Language
Original Title
Series Editor
Series Title
Abbreviated Series Title
Series Volume
Series Issue
Edition
ISSN
0168-1923
ISBN
Medium
Area
Expedition
Conference
Funding
Approved
$loc['no']
Call Number
COAPS @ mfield @
Serial
530
Permanent link to this record
Author
Ramírez-Rodrigues, M.A. ; Alderman, P.D. ; Stefanova, L. ; Cossani, C.M. ; Flores, D. ; Asseng, S.
Title
The value of seasonal forecasts for irrigated, supplementary irrigated, and rainfed wheat cropping systems in northwest Mexico
Type
$loc['typeJournal Article']
Year
2016
Publication
Agricultural Systems
Abbreviated Journal
Agricultural Systems
Volume
147
Issue
Pages
76-86
Keywords
Arid environment ; litigation ; Supplementary irrigation ; Wheat ; Mexico ; Seasonal forecast
Abstract
Address
Corporate Author
Thesis
Publisher
Place of Publication
Editor
Language
Summary Language
Original Title
Series Editor
Series Title
Abbreviated Series Title
Series Volume
Series Issue
Edition
ISSN
0308521X
ISBN
Medium
Area
Expedition
Conference
Funding
Approved
$loc['no']
Call Number
COAPS @ mfield @
Serial
49
Permanent link to this record
Author
Wallcraft, A.J. ; Kara, A.B. ; Hurlburt, H.E. ; Chassignet, E.P. ; Halliwell, G.H.
Title
Value of bulk heat flux parameterizations for ocean SST prediction
Type
$loc['typeJournal Article']
Year
2008
Publication
Journal of Marine Systems
Abbreviated Journal
Journal of Marine Systems
Volume
74
Issue
1-2
Pages
241-258
Keywords
Bulk heat fluxes ; Ocean model SST ; Exchange coefficients ; Atmospheric forcing ; Climate
Abstract
Address
Corporate Author
Thesis
Publisher
Place of Publication
Editor
Language
Summary Language
Original Title
Series Editor
Series Title
Abbreviated Series Title
Series Volume
Series Issue
Edition
ISSN
0924-7963
ISBN
Medium
Area
Expedition
Conference
Funding
Approved
$loc['no']
Call Number
COAPS @ mfield @
Serial
405
Permanent link to this record
Author
Krishnamurti, T.N. ; Jana, S. ; Krishnamurti, R. ; Kumar, V. ; Deepa, R. ; Papa, F. ; Bourassa, M.A. ; Ali, M.M.
Title
Monsoonal intraseasonal oscillations in the ocean heat content over the surface layers of the Bay of Bengal
Type
$loc['typeJournal Article']
Year
2017
Publication
Journal of Marine Systems
Abbreviated Journal
Journal of Marine Systems
Volume
167
Issue
Pages
19-32
Keywords
Intraseasonal oscillations ; Ocean heat content ; Bay of Bengal
Abstract
Address
Corporate Author
Thesis
Publisher
Place of Publication
Editor
Language
Summary Language
Original Title
Series Editor
Series Title
Abbreviated Series Title
Series Volume
Series Issue
Edition
ISSN
0924-7963
ISBN
Medium
Area
Expedition
Conference
Funding
Approved
$loc['no']
Call Number
COAPS @ mfield @
Serial
64
Permanent link to this record
Author
Griffies, S.M. ; Yin, J. ; Durack, P.J. ; Goddard, P. ; Bates, S.C. ; Behrens, E. ; Bentsen, M. ; Bi, D. ; Biastoch, A. ; Böning, C.W. ; Bozec, A. ; Chassignet, E. ; Danabasoglu, G. ; Danilov, S. ; Domingues, C.M. ; Drange, H. ; Farneti, R. ; Fernandez, E. ; Greatbatch, R.J. ; Holland, D.M. ; Ilicak, M. ; Large, W.G. ; Lorbacher, K. ; Lu, J. ; Marsland, S.J. ; Mishra, A. ; George Nurser, A.J. ; Salas y Mélia, D. ; Palter, J.B. ; Samuels, B.L. ; Schröter, J. ; Schwarzkopf, F.U. ; Sidorenko, D. ; Treguier, A.M. ; Tseng, Y.-heng ; Tsujino, H. ; Uotila, P. ; Valcke, S. ; Voldoire, A. ; Wang, Q. ; Winton, M. ; Zhang, X.
Title
An assessment of global and regional sea level for years 1993-2007 in a suite of interannual CORE-II simulations
Type
$loc['typeJournal Article']
Year
2014
Publication
Ocean Modelling
Abbreviated Journal
Ocean Modelling
Volume
78
Issue
Pages
35-89
Keywords
Sea level ; CORE global ocean-ice simulations ; Steric sea level ; Global sea level ; Ocean heat content
Abstract
Address
Corporate Author
Thesis
Publisher
Place of Publication
Editor
Language
Summary Language
Original Title
Series Editor
Series Title
Abbreviated Series Title
Series Volume
Series Issue
Edition
ISSN
1463-5003
ISBN
Medium
Area
Expedition
Conference
Funding
Approved
$loc['no']
Call Number
COAPS @ mfield @
Serial
128
Permanent link to this record
Author
Scott, JP
Title
An Intercomparison of Numerically Modeled Flux Data and Satellite-Derived Flux Data for Warm Seclusions
Type
$loc['typeManuscript']
Year
2011
Publication
Abbreviated Journal
Volume
Issue
Pages
Keywords
Satellite ; Reanalysis ; Air Sea Interaction ; Turbulent Heat Fluxes ; Intercomparison ; Warm Seclusion
Abstract
Address
Corporate Author
Thesis
$loc['Master's thesis']
Publisher
Florida State University
Place of Publication
Tallahassee, FL
Editor
Language
Summary Language
Original Title
Series Editor
Series Title
Abbreviated Series Title
Series Volume
Series Issue
Edition
ISSN
ISBN
Medium
Area
Expedition
Conference
Funding
Approved
$loc['no']
Call Number
COAPS @ mfield @
Serial
335
Permanent link to this record
Author
Hughes, P. J.
Title
North Atlantic Decadal Variability of Ocean Surface Fluxes
Type
$loc['typeManuscript']
Year
2006
Publication
Abbreviated Journal
Volume
Issue
Pages
Keywords
Decadal, North Atlantic, Sensible Heat Flux, Latent Heat Flux, Variability
Abstract
The spatial and temporal variability of the surface turbulent heat fluxes over the North Atlantic is examined using the new objectively produced FSU3 monthly mean 1°x1° gridded wind and surface flux product for 1978-2003. The FSU3 product is constructed from in situ ship and buoy observations via a variational technique. A cost function based on weighted constraints is minimized in the process of determining the surface fluxes. The analysis focuses on a low frequency (basin wide) mode of variability where the latent and sensible heat flux anomalies transition from mainly positive to negative values around 1998. It is hypothesized that the longer time scale variability is linked to changes in the large scale circulation patterns possibly associated with the Atlantic Multidecadal Oscillation (AMO; Schlesinger and Ramankutty 1994, Kerr 2000). The changes in the surface heat fluxes are forced by fluctuations in the mean wind speed. Zonal averages show a clear dissimilarity between the turbulent heat fluxes and wind speed for 1982-1997 and 1998-2003 over the region extending from the equator to roughly 40°N. Larger values are associated with the earlier time period, coinciding with a cool phase of the AMO. The separation between the two time periods is much less evident for the humidity and air/sea temperature differences. The largest differences in the latent heat fluxes, between the two time periods, occur over the tropical, Gulf Stream, and higher latitude regions of the North Atlantic, with magnitudes exceeding 15 Wm-2. The largest sensible heat flux differences are limited to areas along the New England coast and poleward of 40°N.
Address
Department of Meteorology
Corporate Author
Thesis
$loc['Master's thesis']
Publisher
Florida State University
Place of Publication
Tallahassee, FL
Editor
Language
Summary Language
Original Title
Series Editor
Series Title
Abbreviated Series Title
Series Volume
Series Issue
Edition
ISSN
ISBN
Medium
Area
Expedition
Conference
Funding
NOAA, NSF
Approved
$loc['no']
Call Number
COAPS @ mfield @
Serial
617
Permanent link to this record
Author
Guimond, S
Title
Tropical Cyclone Inner-Core Dynamics: A Latent Heat Retrieval and Its Effects on Intensity and Structure Change; and the Impacts of Effective Diffusion on the Axisymmetrization Process
Type
$loc['typeManuscript']
Year
2010
Publication
Abbreviated Journal
Volume
Issue
Pages
Keywords
Hurricanes, Doppler Radar, Latent Heat, Axisymmetrization, Diffusion, Numerical Modeling
Abstract
Despite the fact that latent heating in cloud systems drives many atmospheric circulations, including tropical cyclones, little is known of its magnitude and structure due in large part to inadequate observations. In this work, a reasonably high-resolution (2 km), four-dimensional airborne Doppler radar retrieval of the latent heat of condensation is presented for rapidly intensifying Hurricane Guillermo (1997). Several advancements in the retrieval algorithm are shown including: (1) analyzing the scheme within the dynamically consistent framework of a numerical model, (2) identifying algorithm sensitivities through the use of ancillary data sources and (3) developing a precipitation budget storage term parameterization. The determination of the saturation state is shown to be an important part of the algorithm for updrafts of ~ 5 m s-1 or less. The uncertainties in the magnitude of the retrieved heating are dominated by errors in the vertical velocity. Using a combination of error propagation and Monte Carlo uncertainty techniques, biases were found to be small, and randomly distributed errors in the heating magnitude were ~16 % for updrafts greater than 5 m s-1 and ~156 % for updrafts of 1 m s- 1. The impact of the retrievals is assessed by inserting the heating into realistic numerical simulations at 2 km resolution and comparing the generated wind structure to the Doppler radar observations of Guillermo. Results show that using the latent heat retrievals outperforms a simulation that relies on a state-of-the-art microphysics scheme (Reisner and Jeffery 2009), in terms of wind speed root-mean-square errors, explained variance and eye/eyewall structure. The incorrect transport of water vapor (a function of the sub-grid model and the numerical approximations to advection) and the restrictions on the magnitude of heat release that ensure the present model's stability are suggested as sources of error in the simulation without the retrievals. Motivated by the latent heat retrievals, the dynamics of vortex axisymmetrization from the perspective of thermal anomalies is investigated using an idealized, non-linear atmospheric model (HIGRAD). Attempts at reproducing the results of previous work (Nolan and Grasso 2003; NG03) revealed a discrepancy with the impacts of purely asymmetric forcing. While NG03 found that purely asymmetric heating led to a negligible, largely negative impact on the vortex intensification, in the present study the impacts of asymmetries are found to have an important, largely positive role. Absolute angular momentum budgets revealed that the essential difference between the present work and that of NG03 was the existence of a significant, axisymmetric secondary circulation in the basic-state vortex used in the HIGRAD simulations. This secondary circulation was larger than that present in NG03's simulations. The spin-up of the vortex caused by the asymmetric thermal anomalies was dominated by the axisymmetric fluxes of angular momentum at all times, indicating fundamentally different evolution of asymmetries in the presence of radial flow. Radial momentum budgets were performed to elucidate the mechanisms responsible for the formation of the physically significant secondary circulation. Results show that explicit (sub-grid) diffusion in the model was producing a gradient wind imbalance, which drives a radial inflow and associated secondary circulation in an attempt to re-gain balance. In addition, the production of vorticity anomalies from the asymmetric heating was found to be sensitive to the eddy diffusivity, with large differences between HIGRAD and the widely used WRF model for the exact same value of this uncertain parameter.
Address
Department of Earth, Ocean and Atmospheric Science
Corporate Author
Thesis
$loc['Ph.D. thesis']
Publisher
Florida State University
Place of Publication
Tallahassee, FL
Editor
Language
Summary Language
Original Title
Series Editor
Series Title
Abbreviated Series Title
Series Volume
Series Issue
Edition
ISSN
ISBN
Medium
Area
Expedition
Conference
Funding
Approved
$loc['no']
Call Number
COAPS @ mfield @
Serial
573
Permanent link to this record
Author
Farmer, B
Title
Evaluation of Bulk Heat Fluxes from Atmospheric Datasets
Type
$loc['typeManuscript']
Year
2012
Publication
Abbreviated Journal
Volume
Issue
Pages
Keywords
Comparison ; Data Sets ; Heat Flux ; Linearization
Abstract
Address
Department of Earth Ocean and Atmospheric Sciences
Corporate Author
Thesis
$loc['Master's thesis']
Publisher
Florida State University
Place of Publication
Tallahassee, FL
Editor
Language
Summary Language
Original Title
Series Editor
Series Title
Abbreviated Series Title
Series Volume
Series Issue
Edition
ISSN
ISBN
Medium
Area
Expedition
Conference
Funding
Approved
$loc['no']
Call Number
COAPS @ mfield @
Serial
332
Permanent link to this record
Author
Ali, M. ; Singh, N. ; Kumar, M. ; Zheng, Y. ; Bourassa, M. ; Kishtawal, C. ; Rao, C.
Title
Dominant Modes of Upper Ocean Heat Content in the North Indian Ocean
Type
$loc['typeJournal Article']
Year
2018
Publication
Climate
Abbreviated Journal
Climate
Volume
6
Issue
3
Pages
71
Keywords
ocean heat content ; tropical cyclone heat potential ; dominant modes ; North Indian Ocean ; SUMMER MONSOON ; INTENSIFICATION ; INTENSITY ; PACIFIC
Abstract
The thermal energy needed for the development of hurricanes and monsoons as well as any prolonged marine weather event comes from layers in the upper oceans, not just from the thin layer represented by sea surface temperature alone. Ocean layers have different modes of thermal energy variability because of the different time scales of ocean-atmosphere interaction. Although many previous studies have focused on the influence of upper ocean heat content (OHC) on tropical cyclones and monsoons, no study thus farparticularly in the North Indian Ocean (NIO)has specifically concluded the types of dominant modes in different layers of the ocean. In this study, we examined the dominant modes of variability of OHC of seven layers in the NIO during 1998-2014. We conclude that the thermal variability in the top 50 m of the ocean had statistically significant semiannual and annual modes of variability, while the deeper layers had the annual mode alone. Time series of OHC for the top four layers were analyzed separately for the NIO, Arabian Sea, and Bay of Bengal. For the surface to 50 m layer, the lowest and the highest values of OHC were present in January and May every year, respectively, which was mainly caused by the solar radiation cycle.
Address
Corporate Author
Thesis
Publisher
Place of Publication
Editor
Language
Summary Language
Original Title
Series Editor
Series Title
Abbreviated Series Title
Series Volume
Series Issue
Edition
ISSN
2225-1154
ISBN
Medium
Area
Expedition
Conference
Funding
Approved
$loc['no']
Call Number
COAPS @ rl18 @
Serial
986
Permanent link to this record