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contributor authorReynolds, C. A.
contributor authorPalmer, T. N.
date accessioned2017-06-09T14:35:10Z
date available2017-06-09T14:35:10Z
date copyright1998/10/01
date issued1998
identifier issn0022-4928
identifier otherams-22228.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4158655
description abstractThe full set of kinetic energy singular values and singular vectors for the forward tangent propagator of a quasigeostrophic potential vorticity model is examined. In contrast to the fastest growing singular vectors, the fastest decaying vectors exhibit a downward and downscale transfer of energy and an eastward tilt with height. The near-neutral singular vectors resemble small-scale noise with no localized structure or coherence between levels. Post-time forecast and analysis correction techniques are examined as a function of the number of singular vectors included in the representation of the inverse of the forward tangent propagator. It is found that for the case when the forecast error is known exactly, the best corrections are obtained when using the full inverse, which includes all of the singular vectors. It is also found that the erroneous projection of the analysis uncertainty onto the fastest decaying singular vectors has a significant detrimental effect on the estimation of analysis error. Therefore, for the more realistic case where the forecast error is known imperfectly, use of the full inverse will result in an inaccurate estimate of analysis errors, and the best corrections are obtained when using an inverse composed only of the growing singular vectors. Running the tangent equations with a negative time step is a very good approximation to using the full inverse of the forward tangent propagator.
publisherAmerican Meteorological Society
titleDecaying Singular Vectors and Their Impact on Analysis and Forecast Correction
typeJournal Paper
journal volume55
journal issue19
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1998)055<3005:DSVATI>2.0.CO;2
journal fristpage3005
journal lastpage3023
treeJournal of the Atmospheric Sciences:;1998:;Volume( 055 ):;issue: 019
contenttypeFulltext


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