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    Initial Conditions for Optimal Growth in a Coupled Ocean–Atmosphere Model of ENSO

    Source: Journal of the Atmospheric Sciences:;1998:;Volume( 055 ):;issue: 004::page 537
    Author:
    Thompson, C. J.
    DOI: 10.1175/1520-0469(1998)055<0537:ICFOGI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Several studies have examined the conditions in the equatorial Pacific basin that lead to the maximum growth over a fixed time period, τ. These studies have the purpose of finding the characteristic precursor to an ENSO warm event, or more generally to explore error growth and predictability of the coupled ocean?atmosphere system. This paper develops a linearized version of the Battisti model (similar to the Zebiak?Cane model) with a time-invariant background state. The optimal initial conditions for time period τ (τ-optimals) were computed for a range of τ and for a selection of background states. A number of interesting characteristics of the τ-optimals emerged: 1) The τ-optimals grow more quickly than even the most unstable mode (the ENSO mode) of the system. 2) The τ-optimals develop quickly into the ENSO mode?in around 90 days. 3) The ENSO mode produced by a given τ-optimal does not in general peak at time τ. For τ less than 360 days the ENSO modes peak after time τ, and for τ greater than 360 days the ENSO mode first peaks before τ. At 360 days, designated τmax, the ENSO mode peaks at τ: this is also the τ-optimal, which produces the most growth. 4) Optimals were produced that used the SST only (T-optimals) and that used only the ocean dynamics (r-optimals). It is shown that for τ greater than 60 days, these two optimals both produce ENSO modes (of the same phase). This result makes a comparison of the relative importance of the SST versus the ocean dynamics straightforward: A T-optimal pattern with a 0.1 degree anomaly produces the same size ENSO as an r-optimal pattern with 1.2-m thermocline anomaly. 5) It is shown that the full optimal is the linear combination of these two suboptimals, where their relative sizes are determined by their relative weights (in the norm used). The paper also experiments with a neutral and a damped version of the model and shows that their optimals have similar properties to those listed above; in particular, the shape of the optimal patterns is not overly sensitive to stability. The physical mechanisms for optimal growth are explored in depth.
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      Initial Conditions for Optimal Growth in a Coupled Ocean–Atmosphere Model of ENSO

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    contributor authorThompson, C. J.
    date accessioned2017-06-09T14:34:52Z
    date available2017-06-09T14:34:52Z
    date copyright1998/02/01
    date issued1998
    identifier issn0022-4928
    identifier otherams-22119.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4158534
    description abstractSeveral studies have examined the conditions in the equatorial Pacific basin that lead to the maximum growth over a fixed time period, τ. These studies have the purpose of finding the characteristic precursor to an ENSO warm event, or more generally to explore error growth and predictability of the coupled ocean?atmosphere system. This paper develops a linearized version of the Battisti model (similar to the Zebiak?Cane model) with a time-invariant background state. The optimal initial conditions for time period τ (τ-optimals) were computed for a range of τ and for a selection of background states. A number of interesting characteristics of the τ-optimals emerged: 1) The τ-optimals grow more quickly than even the most unstable mode (the ENSO mode) of the system. 2) The τ-optimals develop quickly into the ENSO mode?in around 90 days. 3) The ENSO mode produced by a given τ-optimal does not in general peak at time τ. For τ less than 360 days the ENSO modes peak after time τ, and for τ greater than 360 days the ENSO mode first peaks before τ. At 360 days, designated τmax, the ENSO mode peaks at τ: this is also the τ-optimal, which produces the most growth. 4) Optimals were produced that used the SST only (T-optimals) and that used only the ocean dynamics (r-optimals). It is shown that for τ greater than 60 days, these two optimals both produce ENSO modes (of the same phase). This result makes a comparison of the relative importance of the SST versus the ocean dynamics straightforward: A T-optimal pattern with a 0.1 degree anomaly produces the same size ENSO as an r-optimal pattern with 1.2-m thermocline anomaly. 5) It is shown that the full optimal is the linear combination of these two suboptimals, where their relative sizes are determined by their relative weights (in the norm used). The paper also experiments with a neutral and a damped version of the model and shows that their optimals have similar properties to those listed above; in particular, the shape of the optimal patterns is not overly sensitive to stability. The physical mechanisms for optimal growth are explored in depth.
    publisherAmerican Meteorological Society
    titleInitial Conditions for Optimal Growth in a Coupled Ocean–Atmosphere Model of ENSO
    typeJournal Paper
    journal volume55
    journal issue4
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1998)055<0537:ICFOGI>2.0.CO;2
    journal fristpage537
    journal lastpage557
    treeJournal of the Atmospheric Sciences:;1998:;Volume( 055 ):;issue: 004
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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