Tools

LEADER 03507cam a2200577Ii 4500

001 ocn902735236;

003 OCoLC;

005 20150728094447.0;

006 m o d ;

007 cr bn|||||||||;

008 150204s2014 ncua ob 000 0 eng d;

035 a| (Sirsi) o902735236;

035 a| (OCoLC)902735236;

043 a| i------;

049 a| EREE;

090 a| QC903.2.I44;

100 1 a| Armstrong, Dicky Leroy,c| Jr.,e| author.?| UNAUTHORIZED;

245 10 a| Influence of climatic oscillations on Indian Ocean tropical cyclone energy /c| by Dicky Leroy Armstrong Jr.;

264 1 a| [Greenville, N.C.] :b| [East Carolina University],c| 2014.;

300 a| 123 pages :b| color illustrations;

336 a| textb| txt2| rdacontent;

337 a| computerb| c2| rdamedia;

338 a| online resourceb| cr2| rdacarrier;

347 a| text fileb| PDFc| 4.87Mb2| rda;

538 a| System requirements: Adobe Reader.;

538 a| Mode of access: World Wide Web.;

502 b| M.A.c| East Carolina Universityd| 2014.;

500 a| Presented to the faculty of the Department of Geography.;

500 a| Advisor: Scott Curtis.;

500 a| Title from PDF t.p. (viewed , 2015).;

520 3 a| Tropical Cyclones form in 4 independent regions of the Indian Ocean Basin ranging from the Arabian Sea, Bay of Bengal, Western South Indian, and Eastern South Indian Ocean. These cyclones lead to distinct patterns in their Accumulated Cyclone Energy for their particular region. The goal of this research article is to examine how the larger scale climate oscillations including ENSO, the Indian Ocean Dipole, and the Subtropical Indian Dipole of the Indian Ocean influence both the patterns in Tropical Cyclone Energy as well as the patterns in the large scale atmosphere of each of the aforementioned sub regions during high ACE events and lower ACE events. This analysis was done using linear regression techniques and appears to reveal the main influence on both ACE and the larger scale atmosphere of the basin is the phases, both warm (El Niño) and cold (La Niña), of the El Niño Southern Oscillation. This is especially true for the northern half of the basin with El Nino leading to higher shear, which is the main weather variable that has an impact on lowering ACE. The other Oscillations appear to have some impact through the placement of their warm pools in the southern portion of the region.;

504 a| Includes bibliographical references.;

650 0 a| Climatic changesz| Indian Ocean Region.=| ^A3535;

650 0 a| Cyclonesz| Indian Ocean Region.=| ^A111964;

650 0 a| Oscillations.=| ^A36601;

650 0 a| Ocean-atmosphere interactionz| Indian Ocean Region.=| ^A45502;

650 0 a| Ocean currentsz| Pacific Ocean.=| ^A140316;

651 0 a| El Niño Current.=| ^A173041;

651 0 a| La Niña Current.=| ^A427790;

653 a| Geography;

653 a| Meteorology;

700 1 a| Curtis, Scottq| (Walter Robert Scott),e| degree supervisor.?| UNAUTHORIZED;

710 2 a| East Carolina University.b| Department of Geography, Planning, and Environment.?| UNAUTHORIZED;

856 40 z| Access via ScholarShipu| http://hdl.handle.net/10342/4640;

949 o| jgml;

994 a| C0b| ERE;

596 a| 1 4;

998 a| 3716344;

999 a| CLICK ON WEB ADDRESSw| ASISc| 1i| 3716344-1001l| JNETm| JOYNERr| Ys| Yt| JNE3ETDu| 2/4/2015x| ETDz| JERESOURCE;

999 a| CLICK ON WEB ADDRESSw| ASISc| 1i| 3716344-2001l| HSLELECm| HSLr| Ys| Yt| HEETDu| 2/4/2015x| ETDz| HERESOURCE;

Influence of climatic oscillations on Indian Ocean tropical cyclone energy / by Dicky Leroy Armstrong Jr.

Author/creator	Armstrong, Dicky Leroy author.
Other author	Curtis, Scott (Walter Robert Scott), degree supervisor.
Other author	East Carolina University. Department of Geography, Planning, and Environment.
Format	Theses and dissertations
Publication	[Greenville, N.C.] : [East Carolina University], 2014.
Description	123 pages : color illustrations
Supplemental Content	Access via ScholarShip
Subjects	Climatic changes--Indian Ocean Region. Cyclones--Indian Ocean Region. Oscillations. Ocean-atmosphere interaction--Indian Ocean Region. Ocean currents--Pacific Ocean. El Niño Current. La Niña Current.

Summary	Tropical Cyclones form in 4 independent regions of the Indian Ocean Basin ranging from the Arabian Sea, Bay of Bengal, Western South Indian, and Eastern South Indian Ocean. These cyclones lead to distinct patterns in their Accumulated Cyclone Energy for their particular region. The goal of this research article is to examine how the larger scale climate oscillations including ENSO, the Indian Ocean Dipole, and the Subtropical Indian Dipole of the Indian Ocean influence both the patterns in Tropical Cyclone Energy as well as the patterns in the large scale atmosphere of each of the aforementioned sub regions during high ACE events and lower ACE events. This analysis was done using linear regression techniques and appears to reveal the main influence on both ACE and the larger scale atmosphere of the basin is the phases, both warm (El Niño) and cold (La Niña), of the El Niño Southern Oscillation. This is especially true for the northern half of the basin with El Nino leading to higher shear, which is the main weather variable that has an impact on lowering ACE. The other Oscillations appear to have some impact through the placement of their warm pools in the southern portion of the region.
General note	Presented to the faculty of the Department of Geography.
General note	Advisor: Scott Curtis.
General note	Title from PDF t.p. (viewed , 2015).
Dissertation note	M.A. East Carolina University 2014.
Bibliography note	Includes bibliographical references.
Technical details	System requirements: Adobe Reader.
Technical details	Mode of access: World Wide Web.

Availability

Library	Location	Call Number	Status	Item Actions
	Electronic Resources	Access Content Online	✔ Available

Influence of climatic oscillations on Indian Ocean tropical cyclone energy / by Dicky Leroy Armstrong Jr.

Click here for more information about this title

Availability