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

Tracking deep-water flow on Eirik Dr...

Henderson, Samuel Straker.

FindBook

Google Book

Amazon

博客來

Tracking deep-water flow on Eirik Drift over the past 160 kyr: Linking deep-water changes to freshwater fluxes.

紀錄類型:	書目-語言資料,印刷品 : Monograph/item
正題名/作者:	Tracking deep-water flow on Eirik Drift over the past 160 kyr: Linking deep-water changes to freshwater fluxes./
作者:	Henderson, Samuel Straker.
面頁冊數:	173 p.
附註:	Source: Dissertation Abstracts International, Volume: 70-03, Section: B, page: 1550.
Contained By:	Dissertation Abstracts International70-03B.
標題:	Geology. -
電子資源:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=3350159
ISBN:	9781109072709

Tracking deep-water flow on Eirik Drift over the past 160 kyr: Linking deep-water changes to freshwater fluxes.
Henderson, Samuel Straker.

Tracking deep-water flow on Eirik Drift over the past 160 kyr: Linking deep-water changes to freshwater fluxes. - 173 p.

Source: Dissertation Abstracts International, Volume: 70-03, Section: B, page: 1550.

Thesis (Ph.D.)--Rutgers The State University of New Jersey - New Brunswick, 2009.

This dissertation uses surface and deep ocean proxies to understand changes in North Atlantic deep-water production associated with periods of increased freshwater input throughout the Late Pleistocene and Holocene. Coring sites on Eirik Drift have long-term sedimentation rates exceeding 15 cm/kyr., allowing for paleoceanographic reconstructions on Milankovitch and millennial time scales.

ISBN: 9781109072709Subjects--Topical Terms:

516570
Geology.

Tracking deep-water flow on Eirik Drift over the past 160 kyr: Linking deep-water changes to freshwater fluxes.
LDR:03419nam 2200325 4500 001 1397036
005 20110705104709.5
008 130515s2009 ||||||||||||||||| ||eng d
020 $a 9781109072709
035 $a (UMI)AAI3350159
035 $a AAI3350159
040 $a UMI $c UMI
100 1 $a Henderson, Samuel Straker. $3 1675848
245 1 0 $a Tracking deep-water flow on Eirik Drift over the past 160 kyr: Linking deep-water changes to freshwater fluxes.
300 $a 173 p.
500 $a Source: Dissertation Abstracts International, Volume: 70-03, Section: B, page: 1550.
500 $a Adviser: James D. Wright.
502 $a Thesis (Ph.D.)--Rutgers The State University of New Jersey - New Brunswick, 2009.
520 $a This dissertation uses surface and deep ocean proxies to understand changes in North Atlantic deep-water production associated with periods of increased freshwater input throughout the Late Pleistocene and Holocene. Coring sites on Eirik Drift have long-term sedimentation rates exceeding 15 cm/kyr., allowing for paleoceanographic reconstructions on Milankovitch and millennial time scales.
520 $a The transition from glacial North Atlantic Intermediate Water (gNAIW) of marine isotope chron (MIC) 2 to North Atlantic Deep Water (NADW) during the Holocene is examined in Chapter 1. Early Holocene (9000-10,500 ka), sedimentation rates in core 21GGC (3471 m) are >100 cm/kyr., indicating gNAIW winnowed upstream glacial sediments, depositing at 21GGC. Enhanced sediment deposition persisted until &sim;9ka when long-term rates leveled off at 40 cm/kyr., indicating NADW density had stabilized. From 8.6 to 8.2 ka, catastrophic drainage of glacial Lake Agassiz poured freshwater into the North Atlantic disrupting deep-ocean circulation.
520 $a Chapter 2 focuses on the past 160 kyr at Site 1306 (2272 m) on the Eirik Drift where highest sedimentation rates occurred during MIC 2- 5d. Mean sortable silt (SS) and delta18O of N. pachyderma (s) are inversely related during this interval, indicating that changes in surface conditions above the Eirik Drift are propagated into the deep ocean. During the past 40 kyr., SS decreases are concomitant with instances of surface ocean freshening. These intervals correlate with Heinrich Events, suggesting that massive ice flows released from the continents altered deep ocean circulation.
520 $a The final chapter examines deep-ocean response during Terminations 1 and 2. Higher insolation forcing across Termination 2 is postulated to promote rapid melting of continental glaciers, leaving little opportunity for continental storage of freshwater. Conversely, lower insolation across Termination 1 allowed continental ice to linger, allowing for the routing and rapid release of freshwater creating abrupt climate reversals (H1, YD and 8.2 kyr Event). Deep-ocean circulation during MIC 5e loses buoyancy in a fashion similar to the Holocene; however, maximum flow velocities are curtailed for &sim;7 kyr after the onset of interglacial conditions. This lag is best explained by the melting of Greenland into areas of NCW convection due to increased insolation forcing.
590 $a School code: 0190.
650 4 $a Geology. $3 516570
650 4 $a Physical Oceanography. $3 1019163
650 4 $a Geochemistry. $3 539092
690 $a 0372
690 $a 0415
690 $a 0996
710 2 $a Rutgers The State University of New Jersey - New Brunswick. $b Graduate School - New Brunswick. $3 1019196
773 0 $t Dissertation Abstracts International $g 70-03B.
790 1 0 $a Wright, James D., $e advisor
790 $a 0190
791 $a Ph.D.
792 $a 2009
856 4 0 $u http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=3350159