Records |
Author  |
Mirhosseini, G.; Srivastava, P.; Stefanova, L. |
Title |
The impact of climate change on rainfall Intensity-Duration-Frequency (IDF) curves in Alabama |
Type |
$loc['typeJournal Article'] |
Year |
2013 |
Publication |
Regional Environmental Change |
Abbreviated Journal |
Reg Environ Change |
Volume |
13 |
Issue |
S1 |
Pages |
25-33 |
Keywords |
Climate change; Intensity–Duration–Frequency (IDF) curve; Temporal downscaling; General Circulation Models (GCMs) |
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Series Volume |
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Series Issue |
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Edition |
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ISSN |
1436-3798 |
ISBN |
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Approved |
$loc['no'] |
Call Number |
COAPS @ mfield @ |
Serial |
221 |
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Author  |
Misra, V.; Bhardwaj, A. |
Title |
Defining the Northeast Monsoon of India |
Type |
$loc['typeJournal Article'] |
Year |
2019 |
Publication |
Monthly Weather Review |
Abbreviated Journal |
Mon. Wea. Rev. |
Volume |
147 |
Issue |
3 |
Pages |
791-807 |
Keywords |
Indian Summer Monsoon, intraseasonal,Climate models, variability, NEM, rainfall |
Abstract |
This study introduces an objective definition for onset and demise of the Northeast Indian Monsoon (NEM). The definition is based on the land surface temperature analysis over the Indian subcontinent. It is diagnosed from the inflection points in the daily anomaly cumulative curve of the area-averaged surface temperature over the provinces of Andhra Pradesh, Rayalseema, and Tamil Nadu located in the southeastern part of India. Per this definition, the climatological onset and demise dates of the NEM season are 6 November and 13 March, respectively. The composite evolution of the seasonal cycle of 850hPa winds, surface wind stress, surface ocean currents, and upper ocean heat content suggest a seasonal shift around the time of the diagnosed onset and demise dates of the NEM season. The interannual variations indicate onset date variations have a larger impact than demise date variations on the seasonal length, seasonal anomalies of rainfall, and surface temperature of the NEM. Furthermore, it is shown that warm El Niño�Southern Oscillation (ENSO) episodes are associated with excess seasonal rainfall, warm seasonal land surface temperature anomalies, and reduced lengths of the NEM season. Likewise, cold ENSO episodes are likely to be related to seasonal deficit rainfall anomalies, cold land surface temperature anomalies, and increased lengths of the NEM season. |
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Language |
English |
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Series Volume |
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Series Issue |
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Edition |
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ISSN |
0027-0644 |
ISBN |
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Medium |
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Area |
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Approved |
$loc['no'] |
Call Number |
COAPS @ rl18 @ |
Serial |
999 |
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Author  |
Misra, V.; Dirmeyer, P.A. |
Title |
Air, Sea, and Land Interactions of the Continental U.S. Hydroclimate |
Type |
$loc['typeJournal Article'] |
Year |
2009 |
Publication |
Journal of Hydrometeorology |
Abbreviated Journal |
J. Hydrometeor |
Volume |
10 |
Issue |
2 |
Pages |
353-373 |
Keywords |
Atmosphere-land interaction; Hydrometeorology; Climatology; Air-sea interaction; Multidecadal variability; Coupled models |
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Series Editor |
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Series Volume |
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Series Issue |
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Edition |
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ISSN |
1525-755X |
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Approved |
$loc['no'] |
Call Number |
COAPS @ mfield @ |
Serial |
664 |
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Author  |
Misra, V.; Mishra, A.; Bhardwaj, A. |
Title |
Simulation of the Intraseasonal Variations of the Indian Summer Monsoon in a Regional Coupled Ocean-Atmosphere Model |
Type |
$loc['typeJournal Article'] |
Year |
2018 |
Publication |
Journal of Climate |
Abbreviated Journal |
J. Climate |
Volume |
31 |
Issue |
8 |
Pages |
3167-3185 |
Keywords |
Asia; Indian Ocean; Mixed layer; Monsoons; Atmosphere-ocean interaction; Regional models |
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Series Issue |
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Edition |
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ISSN |
0894-8755 |
ISBN |
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Medium |
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Area |
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Conference |
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Funding |
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Approved |
$loc['no'] |
Call Number |
COAPS @ mfield @ |
Serial |
557 |
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Author  |
Misra, V.; Mishra, A.; Bhardwaj, A. |
Title |
High-resolution regional-coupled ocean-atmosphere simulation of the Indian Summer Monsoon |
Type |
$loc['typeJournal Article'] |
Year |
2017 |
Publication |
International Journal of Climatology |
Abbreviated Journal |
Int. J. Climatol |
Volume |
37 |
Issue |
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Pages |
717-740 |
Keywords |
monsoon; regional model; ENSO |
Abstract |
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Series Issue |
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Edition |
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ISSN |
0899-8418 |
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Approved |
$loc['no'] |
Call Number |
COAPS @ mfield @ |
Serial |
15 |
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Author  |
Morey, S. L.; Zavala-Hidalgo, J.; O'Brien, J. J. |
Title |
The seasonal variability of continental shelf circulation in the northern and western Gulf of Mexico from a high-resolution numerical model |
Type |
$loc['typeBook Chapter'] |
Year |
2005 |
Publication |
New Developments in the Circulation of the Gulf of Mexico |
Abbreviated Journal |
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Volume |
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Issue |
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Pages |
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Keywords |
Ocean circulation� Mexico, Gulf of� Remote sensing; Ocean circulation� Mexico, Gulf of� Mathematical models |
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Editor |
Sturges, W.; Lugo-Fernandez, A. |
Language |
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Original Title |
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Series Editor |
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Series Title |
Geophys. Mongr. Ser. |
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Series Volume |
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Series Issue |
161 |
Edition |
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ISSN |
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ISBN |
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Area |
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Conference |
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Funding |
ONR, NASA, MMS |
Approved |
$loc['no'] |
Call Number |
COAPS @ mfield @ |
Serial |
852 |
Permanent link to this record |
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Author  |
Morey, S.L. |
Title |
The spring transition from horizontal to vertical thermal stratification on a midlatitude continental shelf |
Type |
$loc['typeJournal Article'] |
Year |
2002 |
Publication |
Journal of Geophysical Research |
Abbreviated Journal |
J. Geophys. Res. |
Volume |
107 |
Issue |
C8 |
Pages |
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Keywords |
continental shelf; stratification; Mixed Layer Dynamics; Coastal Ocean Modeling; West Florida Shelf |
Abstract |
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Series Editor |
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Series Volume |
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Series Issue |
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Edition |
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ISSN |
0148-0227 |
ISBN |
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Approved |
$loc['no'] |
Call Number |
COAPS @ mfield @ |
Serial |
493 |
Permanent link to this record |
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Author  |
Morey, S.L.; Bourassa, M.A.; Dukhovskoy, D.S.; O'Brien, J.J. |
Title |
Modeling studies of the upper ocean response to a tropical cyclone |
Type |
$loc['typeJournal Article'] |
Year |
2006 |
Publication |
Ocean Dynamics |
Abbreviated Journal |
Ocean Dynamics |
Volume |
56 |
Issue |
5-6 |
Pages |
594-606 |
Keywords |
air-sea interaction; tropical cyclones; ocean modeling; air-sea fluxes |
Abstract |
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Series Issue |
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Edition |
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ISSN |
1616-7341 |
ISBN |
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Medium |
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Area |
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Funding |
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Approved |
$loc['no'] |
Call Number |
COAPS @ mfield @ |
Serial |
432 |
Permanent link to this record |
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Author  |
Morey, S.L.; Dukhovskoy, D.S. |
Title |
A downscaling method for simulating deep current interactions with topography – Application to the Sigsbee Escarpment |
Type |
$loc['typeJournal Article'] |
Year |
2013 |
Publication |
Ocean Modelling |
Abbreviated Journal |
Ocean Modelling |
Volume |
69 |
Issue |
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Pages |
50-63 |
Keywords |
Ocean modeling; Model nesting; Topographic flows; USA; Gulf of Mexico; Sigsbee Escarpment |
Abstract |
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Address |
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Corporate Author |
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Thesis |
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Publisher |
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Place of Publication |
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Editor |
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Language |
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Summary Language |
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Original Title |
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Series Editor |
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Abbreviated Series Title |
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Series Volume |
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Series Issue |
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Edition |
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ISSN |
1463-5003 |
ISBN |
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Medium |
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Area |
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Conference |
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Funding |
DeepStar, HYCOM Consortium |
Approved |
$loc['no'] |
Call Number |
COAPS @ mfield @ |
Serial |
183 |
Permanent link to this record |
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Author  |
Morrison, T.; Dukhovskoy, D. S.; McClean, J.; Gille, S. T.; Chassignet, E. |
Title |
Causes of the anomalous heat flux onto the Greenland continental shelf |
Type |
$loc['typeAbstract'] |
Year |
2018 |
Publication |
American Geophysical Union |
Abbreviated Journal |
AGU |
Volume |
Fall Meeting |
Issue |
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Pages |
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Keywords |
0726 Ice sheets, CRYOSPHEREDE: 4207 Arctic and Antarctic oceanography, OCEANOGRAPHY: GENERALDE: 4215 Climate and interannual variability, OCEANOGRAPHY: GENERALDE: 4255 Numerical modeling, OCEANOGRAPHY: GENERAL |
Abstract |
On the continental shelf around Greenland, warm-salty Atlantic water at depth fills the deep narrow fjords where Greenland's tidewater glaciers terminate. Changes in the quantity or properties of this water mass starting in the mid 1990s is thought to be largely responsible for increased ocean-driven melting of the Greenland Ice Sheet. Using high-resolution (nominal 0.1-degree) ocean circulation models we cannot accurately resolve small-scale processes on the shelf or within fjords. However, we can assess changes in the flux of heat via Atlantic water onto the continental shelf. To understand the causes of the anomalous heat that has reached the shelf we examine heat content of subtropical gyre water and shifts in the North Atlantic and Atlantic Multidecadal Oscillations.
We compare changes in heat transport in two eddy permitting simulations: a global 0.1 degree (5-7km around Greenland) resolution coupled hindcast (1970-2009) simulation of the Parallel Ocean Program (POP) and a regional 0.08 degree (3-5km around Greenland) resolution coupled HYbrid Coordinate Ocean Model (HYCOM) hindcast (1993-2016) simulation. Both models are coupled to the Los Alamos National Laboratory Community Ice CodE version 4 and forced by atmospheric reanalysis fluxes. In both models we look for processes that could explain the increase in heat; processes that are present in both are likely to be robust causes of warming. |
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Approved |
$loc['no'] |
Call Number |
COAPS @ user @ |
Serial |
1009 |
Permanent link to this record |