Language:
English
繁體中文
Help
回圖書館首頁
手機版館藏查詢
Login
Back
Switch To:
Labeled
|
MARC Mode
|
ISBD
Atmospheric Responses to Arctic Clim...
~
Koyama, Tomoko.
Linked to FindBook
Google Book
Amazon
博客來
Atmospheric Responses to Arctic Climate Warming: Precipitation, Cyclone, and Synoptic Patterns.
Record Type:
Electronic resources : Monograph/item
Title/Author:
Atmospheric Responses to Arctic Climate Warming: Precipitation, Cyclone, and Synoptic Patterns./
Author:
Koyama, Tomoko.
Published:
Ann Arbor : ProQuest Dissertations & Theses, : 2018,
Description:
167 p.
Notes:
Source: Dissertation Abstracts International, Volume: 79-10(E), Section: B.
Contained By:
Dissertation Abstracts International79-10B(E).
Subject:
Atmospheric sciences. -
Online resource:
http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=10788938
ISBN:
9780355965438
Atmospheric Responses to Arctic Climate Warming: Precipitation, Cyclone, and Synoptic Patterns.
Koyama, Tomoko.
Atmospheric Responses to Arctic Climate Warming: Precipitation, Cyclone, and Synoptic Patterns.
- Ann Arbor : ProQuest Dissertations & Theses, 2018 - 167 p.
Source: Dissertation Abstracts International, Volume: 79-10(E), Section: B.
Thesis (Ph.D.)--University of Colorado at Boulder, 2018.
In recent decades, a rapidly warming lower atmosphere has been observed in the Arctic. Consequently, we wish to address a fundamental question: how do weather patterns in the northern hemisphere respond to these significant changes in the Arctic, especially sea ice loss? To gain insight about the possible linkage between warming Arctic conditions and the resultant atmospheric responses, changes in cyclone activity and synoptic weather patterns were investigated in this study. Given that precipitation can also affect weather patterns, a newly developed reanalysis precipitation was evaluated over Greenland for future hydrological cycle research in the Arctic.
ISBN: 9780355965438Subjects--Topical Terms:
3168354
Atmospheric sciences.
Atmospheric Responses to Arctic Climate Warming: Precipitation, Cyclone, and Synoptic Patterns.
LDR
:02444nmm a2200325 4500
001
2165124
005
20181129115240.5
008
190424s2018 ||||||||||||||||| ||eng d
020
$a
9780355965438
035
$a
(MiAaPQ)AAI10788938
035
$a
(MiAaPQ)colorado:15351
035
$a
AAI10788938
040
$a
MiAaPQ
$c
MiAaPQ
100
1
$a
Koyama, Tomoko.
$3
3353187
245
1 0
$a
Atmospheric Responses to Arctic Climate Warming: Precipitation, Cyclone, and Synoptic Patterns.
260
1
$a
Ann Arbor :
$b
ProQuest Dissertations & Theses,
$c
2018
300
$a
167 p.
500
$a
Source: Dissertation Abstracts International, Volume: 79-10(E), Section: B.
500
$a
Advisers: John Cassano; Julienne Stroeve.
502
$a
Thesis (Ph.D.)--University of Colorado at Boulder, 2018.
520
$a
In recent decades, a rapidly warming lower atmosphere has been observed in the Arctic. Consequently, we wish to address a fundamental question: how do weather patterns in the northern hemisphere respond to these significant changes in the Arctic, especially sea ice loss? To gain insight about the possible linkage between warming Arctic conditions and the resultant atmospheric responses, changes in cyclone activity and synoptic weather patterns were investigated in this study. Given that precipitation can also affect weather patterns, a newly developed reanalysis precipitation was evaluated over Greenland for future hydrological cycle research in the Arctic.
520
$a
First, the Arctic System Reanalysis version 1 precipitation generally showed good agreement with gauge-based precipitation measured in coastal areas. However, precipitation at Summit, Greenland, a higher continental environment, indicated overestimated amounts with respect to Doppler radar measurements.
520
$a
Secondly, no robust changes in cyclone activity were observed, despite the changes in moisture availability, regional baroclinicity, and vertical stability.
520
$a
Lastly, we confirmed that persistent warm surface signals can generate a ridge at 500 hPa and a surface high-pressure system downstream of the ridge. When the Arctic surface forcing has a sufficiently long persistence over a moderately large area, it can induce mid-latitude cold-air advection.
590
$a
School code: 0051.
650
4
$a
Atmospheric sciences.
$3
3168354
690
$a
0725
710
2
$a
University of Colorado at Boulder.
$b
Atmospheric and Oceanic Sciences.
$3
1677746
773
0
$t
Dissertation Abstracts International
$g
79-10B(E).
790
$a
0051
791
$a
Ph.D.
792
$a
2018
793
$a
English
856
4 0
$u
http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=10788938
based on 0 review(s)
Location:
ALL
電子資源
Year:
Volume Number:
Items
1 records • Pages 1 •
1
Inventory Number
Location Name
Item Class
Material type
Call number
Usage Class
Loan Status
No. of reservations
Opac note
Attachments
W9364671
電子資源
11.線上閱覽_V
電子書
EB
一般使用(Normal)
On shelf
0
1 records • Pages 1 •
1
Multimedia
Reviews
Add a review
and share your thoughts with other readers
Export
pickup library
Processing
...
Change password
Login