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Multidecadal Variability in Climate ...
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Oser, Alex.
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Multidecadal Variability in Climate Models and Observations.
紀錄類型:
書目-電子資源 : Monograph/item
正題名/作者:
Multidecadal Variability in Climate Models and Observations./
作者:
Oser, Alex.
出版者:
Ann Arbor : ProQuest Dissertations & Theses, : 2018,
面頁冊數:
62 p.
附註:
Source: Masters Abstracts International, Volume: 80-07.
Contained By:
Masters Abstracts International80-07.
標題:
Climate Change. -
電子資源:
http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=13422428
ISBN:
9780438791572
Multidecadal Variability in Climate Models and Observations.
Oser, Alex.
Multidecadal Variability in Climate Models and Observations.
- Ann Arbor : ProQuest Dissertations & Theses, 2018 - 62 p.
Source: Masters Abstracts International, Volume: 80-07.
Thesis (M.S.)--The University of Wisconsin - Milwaukee, 2018.
This item must not be sold to any third party vendors.
Climate change attribution and prediction using state-of-the-art models continue to garner an ever-growing focus amongst both the scientific community and public alike. Recent analyses showing discrepancies in the structure of modeled and observed decadal climate variability (DCV), therefore, have engendered efforts to not only diagnose the dynamics underpinning observed DCV, but also to characterize the behavior of DCV within climate models. In this thesis, we employ Multichannel Singular Spectrum Analysis (M-SSA) to show that while the DCV signal in observations is best described as a coherent oscillation with complex propagation across the globe, modeled DCV lacks this structure altogether. Specifically, the modeled DCV has a considerably smaller magnitude than its observed counterpart, and tends to exhibit simpler spatiotemporal behaviors. In particular, within the vast majority of models, the DCV structure is best characterized either by globally synchronous, quasi-oscillatory patterns lacking propagation, or, secular trends punctuated with weak, oscillatory-like signals. Both observed and simulated DCV has the largest magnitude in the polar regions. However, the observed anomaly propagation suggests Atlantic control, whereas it is the Arctic that appears to be setting the tone for globally averaged variability in most model runs. Broadly, these results confirm contrasting DCV structure within models and observations, while identifying some qualitative commonalities between the observed and simulated quasi-oscillatory behavior within a few model simulations, thus providing important clues for further DCV research.
ISBN: 9780438791572Subjects--Topical Terms:
894284
Climate Change.
Multidecadal Variability in Climate Models and Observations.
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Climate change attribution and prediction using state-of-the-art models continue to garner an ever-growing focus amongst both the scientific community and public alike. Recent analyses showing discrepancies in the structure of modeled and observed decadal climate variability (DCV), therefore, have engendered efforts to not only diagnose the dynamics underpinning observed DCV, but also to characterize the behavior of DCV within climate models. In this thesis, we employ Multichannel Singular Spectrum Analysis (M-SSA) to show that while the DCV signal in observations is best described as a coherent oscillation with complex propagation across the globe, modeled DCV lacks this structure altogether. Specifically, the modeled DCV has a considerably smaller magnitude than its observed counterpart, and tends to exhibit simpler spatiotemporal behaviors. In particular, within the vast majority of models, the DCV structure is best characterized either by globally synchronous, quasi-oscillatory patterns lacking propagation, or, secular trends punctuated with weak, oscillatory-like signals. Both observed and simulated DCV has the largest magnitude in the polar regions. However, the observed anomaly propagation suggests Atlantic control, whereas it is the Arctic that appears to be setting the tone for globally averaged variability in most model runs. Broadly, these results confirm contrasting DCV structure within models and observations, while identifying some qualitative commonalities between the observed and simulated quasi-oscillatory behavior within a few model simulations, thus providing important clues for further DCV research.
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