語系:
繁體中文
English
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
Global Observations of Physical and ...
~
Hennon, Tyler D.
FindBook
Google Book
Amazon
博客來
Global Observations of Physical and Biogeochemical Processes in the Ocean.
紀錄類型:
書目-電子資源 : Monograph/item
正題名/作者:
Global Observations of Physical and Biogeochemical Processes in the Ocean./
作者:
Hennon, Tyler D.
面頁冊數:
124 p.
附註:
Source: Dissertation Abstracts International, Volume: 78-03(E), Section: B.
Contained By:
Dissertation Abstracts International78-03B(E).
標題:
Physical oceanography. -
電子資源:
http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=10168944
ISBN:
9781369231670
Global Observations of Physical and Biogeochemical Processes in the Ocean.
Hennon, Tyler D.
Global Observations of Physical and Biogeochemical Processes in the Ocean.
- 124 p.
Source: Dissertation Abstracts International, Volume: 78-03(E), Section: B.
Thesis (Ph.D.)--University of Washington, 2016.
We employ numerous global, or semi-global, datasets to observe the large-scale variability of physical and biogeochemical phenomena. In Chapter 1, we use Argo floats to estimate the vertical displacement of internal gravity waves. Internal wave intensity is found to be positively correlated with bathymetric roughness and proximity to the seafloor. The global variability of internal wave intensity also strongly resembles patterns of diapycnal diffusivity established by prior studies, suggesting breaking internal waves are largely responsible for abyssal mixing. In Chapter 2, we use Argo floats equipped with dissolved oxygen sensors to measure oxygen drawdown beneath the mixed layer, which is representative of respiration and remineralization of organic matter. We observe strong regional variability across the eight locations examined. Depth-integrated respiration is used as a lower-bound for organic carbon exported from the surface ocean. We find that carbon export and export efficiency is low at weakly seasonal locations, and high at strongly seasonal locations. In Chapter 3, we use a variety of datasets to construct composite averages of mesoscale eddy characteristics. By using repeat hydrography, we are able to estimate the nitrate anomaly within the interior of eddies. Additionally, satellite observations allow us to estimate the chlorophyll anomaly at the surface. By combining subsurface and surface observations, we examine how the nitrate anomaly covaries with the chlorophyll anomaly. Although our observations only allow us to explore global variability very coarsely, we find that the influence of mesoscale eddies on nutrients and chlorophyll is significantly different at low-, mid-, and high-latitude.
ISBN: 9781369231670Subjects--Topical Terms:
3168433
Physical oceanography.
Global Observations of Physical and Biogeochemical Processes in the Ocean.
LDR
:02633nmm a2200289 4500
001
2115301
005
20170228070019.5
008
180830s2016 ||||||||||||||||| ||eng d
020
$a
9781369231670
035
$a
(MiAaPQ)AAI10168944
035
$a
AAI10168944
040
$a
MiAaPQ
$c
MiAaPQ
100
1
$a
Hennon, Tyler D.
$3
3276943
245
1 0
$a
Global Observations of Physical and Biogeochemical Processes in the Ocean.
300
$a
124 p.
500
$a
Source: Dissertation Abstracts International, Volume: 78-03(E), Section: B.
500
$a
Adviser: Stephen C. Riser.
502
$a
Thesis (Ph.D.)--University of Washington, 2016.
520
$a
We employ numerous global, or semi-global, datasets to observe the large-scale variability of physical and biogeochemical phenomena. In Chapter 1, we use Argo floats to estimate the vertical displacement of internal gravity waves. Internal wave intensity is found to be positively correlated with bathymetric roughness and proximity to the seafloor. The global variability of internal wave intensity also strongly resembles patterns of diapycnal diffusivity established by prior studies, suggesting breaking internal waves are largely responsible for abyssal mixing. In Chapter 2, we use Argo floats equipped with dissolved oxygen sensors to measure oxygen drawdown beneath the mixed layer, which is representative of respiration and remineralization of organic matter. We observe strong regional variability across the eight locations examined. Depth-integrated respiration is used as a lower-bound for organic carbon exported from the surface ocean. We find that carbon export and export efficiency is low at weakly seasonal locations, and high at strongly seasonal locations. In Chapter 3, we use a variety of datasets to construct composite averages of mesoscale eddy characteristics. By using repeat hydrography, we are able to estimate the nitrate anomaly within the interior of eddies. Additionally, satellite observations allow us to estimate the chlorophyll anomaly at the surface. By combining subsurface and surface observations, we examine how the nitrate anomaly covaries with the chlorophyll anomaly. Although our observations only allow us to explore global variability very coarsely, we find that the influence of mesoscale eddies on nutrients and chlorophyll is significantly different at low-, mid-, and high-latitude.
590
$a
School code: 0250.
650
4
$a
Physical oceanography.
$3
3168433
650
4
$a
Biogeochemistry.
$3
545717
650
4
$a
Geophysics.
$3
535228
690
$a
0415
690
$a
0425
690
$a
0373
710
2
$a
University of Washington.
$b
Oceanography.
$3
2101461
773
0
$t
Dissertation Abstracts International
$g
78-03B(E).
790
$a
0250
791
$a
Ph.D.
792
$a
2016
793
$a
English
856
4 0
$u
http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=10168944
筆 0 讀者評論
館藏地:
全部
電子資源
出版年:
卷號:
館藏
1 筆 • 頁數 1 •
1
條碼號
典藏地名稱
館藏流通類別
資料類型
索書號
使用類型
借閱狀態
預約狀態
備註欄
附件
W9325922
電子資源
01.外借(書)_YB
電子書
EB
一般使用(Normal)
在架
0
1 筆 • 頁數 1 •
1
多媒體
評論
新增評論
分享你的心得
Export
取書館
處理中
...
變更密碼
登入