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Atmosphere-Surface Coupling in the Marginal Ice Zone: The Influence of Surface Heterogeneity
Atmosphere-Surface Coupling in the Marginal Ice Zone: The Influence of Surface Heterogeneity
상세정보
- 자료유형
- 학위논문 서양
- 최종처리일시
- 20250211151450
- ISBN
- 9798382807126
- DDC
- 551.5
- 서명/저자
- Atmosphere-Surface Coupling in the Marginal Ice Zone: The Influence of Surface Heterogeneity
- 발행사항
- [Sl] : Princeton University, 2024
- 발행사항
- Ann Arbor : ProQuest Dissertations & Theses, 2024
- 형태사항
- 150 p
- 주기사항
- Source: Dissertations Abstracts International, Volume: 85-12, Section: B.
- 주기사항
- Advisor: Bou-Zeid, Elie.
- 학위논문주기
- Thesis (Ph.D.)--Princeton University, 2024.
- 초록/해제
- 요약Climate models underestimate Arctic sea ice loss through ocean-atmospheric interactions that are improperly modeled. One reason for this disconnect is the heterogeneity of sea ice in the marginal ice zone (MIZ), causing secondary circulations unable to be captured by climate models within the boundary layer over the MIZ (MIZ-ABL). Large-eddy simulations of the MIZ-ABL were conducted throughout this study to understand how surface-atmosphere fluxes, as well as the dynamics and thermodynamics of the boundary layer, change as the geometric pattern of sea ice changes. A simplified theoretical framework was proposed to non-dimensionalize the dynamics of the MIZ-ABL; this method captured the surface thermodynamics reasonably well, however, they were unable to predict the atmospheric dynamics, suggesting that the individual stabilities over each surface influence the dynamics separately.A suite of large-eddy simulations over idealized surface patterns (with equivalent ice fraction and average floe area) were used to demonstrate that spatial organization plays a crucial role in determining boundary-layer structure. A broader set of surface characterization metrics was then established, minimized, and analyzed (ice fraction, patch density, splitting index, and perimeter-area fractal dimension), detailing the first steps towards further development of methods to quantify the variability of binary surfaces. A method was then proposed to obtain a principal orientation of the surface relative to the mean wind. Real-world sea ice patterns were then simulated, showing that the ice fraction and geostrophic wind direction are not enough to predict bulk surface thermodynamic fluxes. Another simulation suite of real-world satellite-sensed sea ice maps were conducted to understand how each metric affects the MIZ-ABL. Roughness heterogeneity showed minimal contributions to the resulting atmospheric circulations, and a multi-linear regression of such features, with discussion on how future models may be generated, was presented in the context of climate modeling.While this study furthers the work on thermally heterogeneous surfaces and the secondary circulations in the MIZ-ABL, this work opens as many questions as it answers, encouraging future studies to examine methods for quantifying binary surfaces in the context of rapid stabilizing and destabilizing transitions.
- 일반주제명
- Atmospheric sciences
- 일반주제명
- Fluid mechanics
- 기타저자
- Princeton University Civil and Environmental Engineering
- 기본자료저록
- Dissertations Abstracts International. 85-12B.
- 전자적 위치 및 접속
- 로그인 후 원문을 볼 수 있습니다.
MARC
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■00520250211151450
■006m o d
■007cr#unu||||||||
■020 ▼a9798382807126
■035 ▼a(MiAaPQ)AAI31296728
■040 ▼aMiAaPQ▼cMiAaPQ
■0820 ▼a551.5
■1001 ▼aFogarty, Joseph J.▼0(orcid)0009-0008-3374-5232
■24510▼aAtmosphere-Surface Coupling in the Marginal Ice Zone: The Influence of Surface Heterogeneity
■260 ▼a[Sl]▼bPrinceton University▼c2024
■260 1▼aAnn Arbor▼bProQuest Dissertations & Theses▼c2024
■300 ▼a150 p
■500 ▼aSource: Dissertations Abstracts International, Volume: 85-12, Section: B.
■500 ▼aAdvisor: Bou-Zeid, Elie.
■5021 ▼aThesis (Ph.D.)--Princeton University, 2024.
■520 ▼aClimate models underestimate Arctic sea ice loss through ocean-atmospheric interactions that are improperly modeled. One reason for this disconnect is the heterogeneity of sea ice in the marginal ice zone (MIZ), causing secondary circulations unable to be captured by climate models within the boundary layer over the MIZ (MIZ-ABL). Large-eddy simulations of the MIZ-ABL were conducted throughout this study to understand how surface-atmosphere fluxes, as well as the dynamics and thermodynamics of the boundary layer, change as the geometric pattern of sea ice changes. A simplified theoretical framework was proposed to non-dimensionalize the dynamics of the MIZ-ABL; this method captured the surface thermodynamics reasonably well, however, they were unable to predict the atmospheric dynamics, suggesting that the individual stabilities over each surface influence the dynamics separately.A suite of large-eddy simulations over idealized surface patterns (with equivalent ice fraction and average floe area) were used to demonstrate that spatial organization plays a crucial role in determining boundary-layer structure. A broader set of surface characterization metrics was then established, minimized, and analyzed (ice fraction, patch density, splitting index, and perimeter-area fractal dimension), detailing the first steps towards further development of methods to quantify the variability of binary surfaces. A method was then proposed to obtain a principal orientation of the surface relative to the mean wind. Real-world sea ice patterns were then simulated, showing that the ice fraction and geostrophic wind direction are not enough to predict bulk surface thermodynamic fluxes. Another simulation suite of real-world satellite-sensed sea ice maps were conducted to understand how each metric affects the MIZ-ABL. Roughness heterogeneity showed minimal contributions to the resulting atmospheric circulations, and a multi-linear regression of such features, with discussion on how future models may be generated, was presented in the context of climate modeling.While this study furthers the work on thermally heterogeneous surfaces and the secondary circulations in the MIZ-ABL, this work opens as many questions as it answers, encouraging future studies to examine methods for quantifying binary surfaces in the context of rapid stabilizing and destabilizing transitions.
■590 ▼aSchool code: 0181.
■650 4▼aAtmospheric sciences
■650 4▼aFluid mechanics
■650 4▼aEnvironmental engineering
■653 ▼aAtmospheric boundary layer
■653 ▼aMarginal ice zone
■653 ▼aSurface heterogeneity
■653 ▼aSurface-atmosphere fluxes
■690 ▼a0725
■690 ▼a0775
■690 ▼a0204
■71020▼aPrinceton University▼bCivil and Environmental Engineering.
■7730 ▼tDissertations Abstracts International▼g85-12B.
■790 ▼a0181
■791 ▼aPh.D.
■792 ▼a2024
■793 ▼aEnglish
■85640▼uhttp://www.riss.kr/pdu/ddodLink.do?id=T17161829▼nKERIS▼z이 자료의 원문은 한국교육학술정보원에서 제공합니다.
