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
FindBook
Google Book
Amazon
博客來
A Study on the Atmospheric, Cryospheric, and Hydrologic Processes Governing the Evolution of Regional Hydroclimates.
紀錄類型:
書目-電子資源 : Monograph/item
正題名/作者:
A Study on the Atmospheric, Cryospheric, and Hydrologic Processes Governing the Evolution of Regional Hydroclimates./
作者:
Minallah, Samar.
面頁冊數:
1 online resource (237 pages)
附註:
Source: Dissertations Abstracts International, Volume: 84-04, Section: A.
Contained By:
Dissertations Abstracts International84-04A.
標題:
Hydrologic sciences. -
電子資源:
http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=29712410click for full text (PQDT)
ISBN:
9798845452566
A Study on the Atmospheric, Cryospheric, and Hydrologic Processes Governing the Evolution of Regional Hydroclimates.
Minallah, Samar.
A Study on the Atmospheric, Cryospheric, and Hydrologic Processes Governing the Evolution of Regional Hydroclimates.
- 1 online resource (237 pages)
Source: Dissertations Abstracts International, Volume: 84-04, Section: A.
Thesis (Ph.D.)--University of Michigan, 2022.
Includes bibliographical references
Regional hydroclimates constitute the interplay between climate, weather, and water resources at sub-continental scales. They continually evolve by responding to changes and perturbations in global climate, water cycle, and terrestrial surface and subsurface processes. This dissertation is on region-specific and process-based assessments of the atmosphere, cryosphere, and hydrosphere interactions to understand the mechanisms driving variability in hydroclimates. The overarching motivation is to quantify the availability of water within the Earth's components and understand how water systems evolve in space and time. This research combines data analysis and modeling tools with fundamental physical laws to study two distinct systems - large inland lakes and mountain glaciers - both critical water resources for societies, economies, and ecosystems. In the first study, we discuss how large inland water bodies regulate the water cycle for three geographical regions: the African Great Lakes, the Laurentian Great Lakes, and Lake Baikal. We found that these lakes control regional micro- and meso-scale weather and climate, and different modeled lake representations can simulate markedly different coupled lake-atmosphere processes. The second study analyses the atmospheric moisture budget in the Laurentian Great Lakes region. We developed process-level understanding of the precipitation seasonality and established the role of lakes in inducing differences in the water cycle seasonality. These lakes are a source of moisture through evaporation and generate localized moisture flux convergence/divergence patterns. We further quantified the future changes in the budget using Coupled Model Intercomparison Project (CMIP6) data. There are common patterns of change in the mid-century (2041 - 2070) projections of climate variables, specifically, an increase in evapotranspiration throughout the year and intensification of winter/spring precipitation, indicating a shift in the precipitation seasonal cycle towards the colder months. The next chapter delves into land surface hydrology, specifically looking at the controls of variability in the terrestrial water budget using a high-resolution model for the Laurentian Great Lakes domain. This is a hydrologically heterogeneous region, with various regulators of the water budget at different timescales. At higher latitudes, snowpack and soil moisture are the principal drivers of variability, while at lower latitudes precipitation, evapotranspiration, and runoff are the dominant controls of budget variability. The subsequent work centers on mountain cryosphere to study the evolution of Karakoram glaciers using a numerical model. We explored the relation between climate, mass balance, and ice dynamics in driving glacier geometry (length, thickness, area, and volume) changes. We found that similar climate forcing can trigger radically different responses, even in neighboring glaciers, and changes in area and length do not always correspond to a similar change in the glacial volume. We also applied a new approach to calibrate ice dynamics parameters and introduced a novel scheme for dynamic spin-up to match geodetic mass balance observations while accounting for changing glacier area. In the final chapter, the dissertation lays the groundwork to simulate three-dimensional dynamics of mountain glaciers using the Community Ice Sheet Model to advance the field of glaciology as a coupled process within the larger Earth system modeling framework. Throughout this dissertation, we highlight the significance of understanding the governing processes modulating regional hydroclimates before assessing their future evolution, and the importance of effectively representing water/ice reservoirs in numerical models. This is critical to improve accuracy and reliability of future climate assessments using models which currently have limitations in simulating regional-scale climate.
Electronic reproduction.
Ann Arbor, Mich. :
ProQuest,
2023
Mode of access: World Wide Web
ISBN: 9798845452566Subjects--Topical Terms:
3168407
Hydrologic sciences.
Subjects--Index Terms:
Earth system scienceIndex Terms--Genre/Form:
542853
Electronic books.
A Study on the Atmospheric, Cryospheric, and Hydrologic Processes Governing the Evolution of Regional Hydroclimates.
LDR
:05555nmm a2200457K 4500
001
2358519
005
20230814100738.5
006
m o d
007
cr mn ---uuuuu
008
241011s2022 xx obm 000 0 eng d
020
$a
9798845452566
035
$a
(MiAaPQ)AAI29712410
035
$a
(MiAaPQ)umichrackham004455
035
$a
AAI29712410
040
$a
MiAaPQ
$b
eng
$c
MiAaPQ
$d
NTU
100
1
$a
Minallah, Samar.
$3
3699053
245
1 2
$a
A Study on the Atmospheric, Cryospheric, and Hydrologic Processes Governing the Evolution of Regional Hydroclimates.
264
0
$c
2022
300
$a
1 online resource (237 pages)
336
$a
text
$b
txt
$2
rdacontent
337
$a
computer
$b
c
$2
rdamedia
338
$a
online resource
$b
cr
$2
rdacarrier
500
$a
Source: Dissertations Abstracts International, Volume: 84-04, Section: A.
500
$a
Advisor: Bassis, Jeremy N.; Steiner, Allison L.
502
$a
Thesis (Ph.D.)--University of Michigan, 2022.
504
$a
Includes bibliographical references
520
$a
Regional hydroclimates constitute the interplay between climate, weather, and water resources at sub-continental scales. They continually evolve by responding to changes and perturbations in global climate, water cycle, and terrestrial surface and subsurface processes. This dissertation is on region-specific and process-based assessments of the atmosphere, cryosphere, and hydrosphere interactions to understand the mechanisms driving variability in hydroclimates. The overarching motivation is to quantify the availability of water within the Earth's components and understand how water systems evolve in space and time. This research combines data analysis and modeling tools with fundamental physical laws to study two distinct systems - large inland lakes and mountain glaciers - both critical water resources for societies, economies, and ecosystems. In the first study, we discuss how large inland water bodies regulate the water cycle for three geographical regions: the African Great Lakes, the Laurentian Great Lakes, and Lake Baikal. We found that these lakes control regional micro- and meso-scale weather and climate, and different modeled lake representations can simulate markedly different coupled lake-atmosphere processes. The second study analyses the atmospheric moisture budget in the Laurentian Great Lakes region. We developed process-level understanding of the precipitation seasonality and established the role of lakes in inducing differences in the water cycle seasonality. These lakes are a source of moisture through evaporation and generate localized moisture flux convergence/divergence patterns. We further quantified the future changes in the budget using Coupled Model Intercomparison Project (CMIP6) data. There are common patterns of change in the mid-century (2041 - 2070) projections of climate variables, specifically, an increase in evapotranspiration throughout the year and intensification of winter/spring precipitation, indicating a shift in the precipitation seasonal cycle towards the colder months. The next chapter delves into land surface hydrology, specifically looking at the controls of variability in the terrestrial water budget using a high-resolution model for the Laurentian Great Lakes domain. This is a hydrologically heterogeneous region, with various regulators of the water budget at different timescales. At higher latitudes, snowpack and soil moisture are the principal drivers of variability, while at lower latitudes precipitation, evapotranspiration, and runoff are the dominant controls of budget variability. The subsequent work centers on mountain cryosphere to study the evolution of Karakoram glaciers using a numerical model. We explored the relation between climate, mass balance, and ice dynamics in driving glacier geometry (length, thickness, area, and volume) changes. We found that similar climate forcing can trigger radically different responses, even in neighboring glaciers, and changes in area and length do not always correspond to a similar change in the glacial volume. We also applied a new approach to calibrate ice dynamics parameters and introduced a novel scheme for dynamic spin-up to match geodetic mass balance observations while accounting for changing glacier area. In the final chapter, the dissertation lays the groundwork to simulate three-dimensional dynamics of mountain glaciers using the Community Ice Sheet Model to advance the field of glaciology as a coupled process within the larger Earth system modeling framework. Throughout this dissertation, we highlight the significance of understanding the governing processes modulating regional hydroclimates before assessing their future evolution, and the importance of effectively representing water/ice reservoirs in numerical models. This is critical to improve accuracy and reliability of future climate assessments using models which currently have limitations in simulating regional-scale climate.
533
$a
Electronic reproduction.
$b
Ann Arbor, Mich. :
$c
ProQuest,
$d
2023
538
$a
Mode of access: World Wide Web
650
4
$a
Hydrologic sciences.
$3
3168407
650
4
$a
Climate change.
$2
bicssc
$3
2079509
650
4
$a
Atmospheric sciences.
$3
3168354
650
4
$a
Water resources management.
$3
794747
650
4
$a
Regional studies.
$3
3173672
653
$a
Earth system science
653
$a
Water cycle
653
$a
Inland water bodies
653
$a
Mountain glaciers
653
$a
Numerical models
653
$a
Conservation laws
653
$a
Regional hydroclimates
655
7
$a
Electronic books.
$2
lcsh
$3
542853
690
$a
0725
690
$a
0388
690
$a
0404
690
$a
0595
690
$a
0604
710
2
$a
ProQuest Information and Learning Co.
$3
783688
710
2
$a
University of Michigan.
$b
Climate and Space Sciences and Engineering.
$3
3560685
773
0
$t
Dissertations Abstracts International
$g
84-04A.
856
4 0
$u
http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=29712410
$z
click for full text (PQDT)
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
W9480875
電子資源
11.線上閱覽_V
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