東華大學圖書館 |

語系: 繁體中文

說明(常見問題)

回圖書館首頁

手機版館藏查詢

登入

回首頁

切換: 標籤 | MARC模式 | ISBD

Structure and Dynamics of the Gulf S...

Sanchez Franks, Alejandra.

FindBook

Google Book

Amazon

博客來

Structure and Dynamics of the Gulf Stream's Interannual Migration East of Cape Hatteras.

紀錄類型:	書目-電子資源 : Monograph/item
正題名/作者:	Structure and Dynamics of the Gulf Stream's Interannual Migration East of Cape Hatteras./
作者:	Sanchez Franks, Alejandra.
面頁冊數:	113 p.
附註:	Source: Dissertation Abstracts International, Volume: 76-11(E), Section: B.
Contained By:	Dissertation Abstracts International76-11B(E).
標題:	Physical oceanography. -
電子資源:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=3715890
ISBN:	9781321942187

Structure and Dynamics of the Gulf Stream's Interannual Migration East of Cape Hatteras.
Sanchez Franks, Alejandra.

Structure and Dynamics of the Gulf Stream's Interannual Migration East of Cape Hatteras. - 113 p.

Source: Dissertation Abstracts International, Volume: 76-11(E), Section: B.

Thesis (Ph.D.)--State University of New York at Stony Brook, 2015.

The Gulf Stream's (GS) main mode of interannual variability, its latitudinal migration, has been shown to be atmospherically forced by the North Atlantic Oscillation (NAO), taking a 2 year lag into account. Observational and model data were used here to examine the structure of the GS's migration and the dynamics linking it to atmospheric forcing.

ISBN: 9781321942187Subjects--Topical Terms:

3168433
Physical oceanography.

Structure and Dynamics of the Gulf Stream's Interannual Migration East of Cape Hatteras.
LDR:04168nmm a2200349 4500 001 2072572
005 20160808081000.5
008 170521s2015 ||||||||||||||||| ||eng d
020 $a 9781321942187
035 $a (MiAaPQ)AAI3715890
035 $a AAI3715890
040 $a MiAaPQ $c MiAaPQ
100 1 $a Sanchez Franks, Alejandra. $3 3187773
245 1 0 $a Structure and Dynamics of the Gulf Stream's Interannual Migration East of Cape Hatteras.
300 $a 113 p.
500 $a Source: Dissertation Abstracts International, Volume: 76-11(E), Section: B.
500 $a Advisers: Charles N. Flagg; Robert Wilson.
502 $a Thesis (Ph.D.)--State University of New York at Stony Brook, 2015.
520 $a The Gulf Stream's (GS) main mode of interannual variability, its latitudinal migration, has been shown to be atmospherically forced by the North Atlantic Oscillation (NAO), taking a 2 year lag into account. Observational and model data were used here to examine the structure of the GS's migration and the dynamics linking it to atmospheric forcing.
520 $a The structure of the GS's interannual variability was investigated from different measures of GS position and transport at 38°N and 27°N (i.e. the Florida Current). Using a zonally averaged index, the local measurements of GS position at 38°N proved good representations of overall meridional shifting of the current. GS position and transport were shown linked to the NAO, though the relationship between the GS and the Florida Current transport was not found statistically significant. This indicated that the Florida Current does not have a detectable interannual signal downstream in the GS.
520 $a Further investigation of the link between GS position and the NAO revealed the GS position has a more robust correlation with the Icelandic Low (IL) component of the NAO rather than with the NAO itself. Using Sea Surface temperature composites, it was shown that for anomalously low (west) IL pressure (longitude) corresponding to cooler surface temperatures in the Labrador Sea the GS position shifts north after a period of &sim;2 years. The relationship between GS and IL pressure (longitude) was further used to create a forecasting scheme for GS position one year ahead of time. The correlation between the resulting forecasted GS and the observed GS was 0.60, significant at 95% level.
520 $a Insight into the 2-year delay between the GS and atmospheric forcing was obtained from mean structure and interannual variability of the Slope Sea and Labrador Current. Observations suggested there is a statistically significant link between the Labrador Current, the Slope Sea, and GS position. On 0.5 to 1 year time scales, increases (decreases) in Slope Sea transport lags southward (northward) shifts in GS position by 1 year (r=0.48, significant at 95% level), and cooler (warmer) SSTs in the Slope Sea lead southward (northward) shifts in GS position by 0.5 years (r=0.65, significant at 95% level). On longer time scales, Labrador Current transport and GS position are found significantly correlated (r=-0.68, significant at 95% level) where increases in Labrador Current transport lead southern shifts in GS position taking a 2 year lag into account.
520 $a Finally, the connection between GS position, the Atlantic meridional overturning circulation (AMOC) and the regional biogeochemical cycle was investigated using coupled climate models and ocean temperature observations. GS position and the AMOC simulated from GFDL's Climate Model 2.1 found enhanced (weakened) AMOC significantly correlated with south (north) shifts in GS position on decadal time scale. Similarly, results from the GFDL Earth System Models indicated an enhanced (weakened) AMOC leads southward (northward) displacements in GS position and increases (decreases) in regional chlorophyll and nutrient concentrations.
590 $a School code: 0771.
650 4 $a Physical oceanography. $3 3168433
650 4 $a Atmospheric sciences. $3 3168354
650 4 $a Biogeochemistry. $3 545717
650 4 $a Geophysics. $3 535228
690 $a 0415
690 $a 0725
690 $a 0425
690 $a 0373
710 2 $a State University of New York at Stony Brook. $b Marine and Atmospheric Science. $3 1683777
773 0 $t Dissertation Abstracts International $g 76-11B(E).
790 $a 0771
791 $a Ph.D.
792 $a 2015
793 $a English
856 4 0 $u http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=3715890