91 research outputs found
On the mechanisms of late 20th century sea-surface temperature trends over the Antarctic Circumpolar Current
The Antarctic Circumpolar Current (ACC), with its associated three-dimensional circulation, plays an important role in global climate. This study concentrates on surface signatures of recent climate change in the ACC region and on mechanisms that contro
Ocean eddy dynamics in a coupled ocean-atmosphere model
Author Posting. © American Meteorological Society, 2007. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Journal of Physical Oceanography 37 (2007): 1103-1121, doi:10.1175/jpo3041.1.The role of mesoscale oceanic eddies is analyzed in a quasigeostrophic coupled ocean–atmosphere model operating at a large Reynolds number. The model dynamics are characterized by decadal variability that involves nonlinear adjustment of the ocean to coherent north–south shifts of the atmosphere. The oceanic eddy effects are diagnosed by the dynamical decomposition method adapted for nonstationary external forcing. The main effects of the eddies are an enhancement of the oceanic eastward jet separating the subpolar and subtropical gyres and a weakening of the gyres. The flow-enhancing effect is due to nonlinear rectification driven by fluctuations of the eddy forcing. This is a nonlocal process involving generation of the eddies by the flow instabilities in the western boundary current and the upstream part of the eastward jet. The eddies are advected by the mean current to the east, where they backscatter into the rectified enhancement of the eastward jet. The gyre-weakening effect, which is due to the time-mean buoyancy component of the eddy forcing, is a result of the baroclinic instability of the westward return currents. The diagnosed eddy forcing is parameterized in a non-eddy-resolving ocean model, as a nonstationary random process, in which the corresponding parameters are derived from the control coupled simulation. The key parameter of the random process—its variance—is related to the large-scale flow baroclinicity index. It is shown that the coupled model with the non-eddy-resolving ocean component and the parameterized eddies correctly simulates climatology and low-frequency variability of the control eddy-resolving coupled solution.Funding for this work came from NSF Grants
OCE 02-221066 and OCE 03-44094. Additional funding
for PB was provided by the U.K. Royal Society Fellowship
and by WHOI Grants 27100056 and 52990035
A mechanistic model of mid-latitude decadal climate variability
Author Posting. © Elsevier B.V., 2007. This is the author's version of the work. It is posted here by permission of Elsevier B.V. for personal use, not for redistribution. The definitive version was published in Physica D: Nonlinear Phenomena 237 (2008): 584-599, doi:10.1016/j.physd.2007.09.025.A simple heuristic model of coupled decadal ocean–atmosphere modes in middle
latitudes is developed. Previous studies have treated atmospheric intrinsic variability
as a linear stochastic process modified by a deterministic coupling to the ocean.
The present paper takes an alternative view: based on observational, as well as
process modeling results, it represents this variability in terms of irregular transitions
between two anomalously persistent, high-latitude and low-latitude jet-stream
states. Atmospheric behavior is thus governed by an equation analogous to that describing
the trajectory of a particle in a double-well potential, subject to stochastic
forcing. Oceanic adjustment to a positional shift in the atmospheric jet involves
persistent circulation anomalies maintained by the action of baroclinic eddies; this
process is parameterized in the model as a delayed oceanic response. The associated
sea-surface temperature anomalies provide heat fluxes that affect atmospheric
circulation by modifying the shape of the double-well potential. If the latter coupling
is strong enough, the model’s spectrum exhibits a peak at a periodicity related
to the ocean’s eddy-driven adjustment time. A nearly analytical approximation of
the coupled model is used to study the sensitivity of this behavior to key model
parameters.This research
was supported by National Science Foundation grant OCE-02-221066 (all coauthors)
and the Department of Energy grant DE-FG-03-01ER63260 (MG
and SK)
North Atlantic climate variability in coupled models and data
© 2008 The Authors. This work is licensed
under a Creative Commons Attribution License. The definitive version was published in Nonlinear Processes in Geophysics 15 (2008): 13-24, doi:10.5194/npg-15-13-2008We show that the observed zonally averaged jet in the Northern Hemisphere atmosphere exhibits two spatial patterns with broadband variability in the decadal and inter-decadal range; these patterns are consistent with an important role of local, mid-latitude ocean–atmosphere coupling. A key aspect of this behaviour is the fundamentally nonlinear bi-stability of the atmospheric jet's latitudinal position, which enables relatively small sea-surface temperature anomalies associated with ocean processes to affect the large-scale atmospheric winds. The wind anomalies induce, in turn, complex three-dimensional anomalies in the ocean's main thermocline; in particular, they may be responsible for recently reported cooling of the upper ocean. Both observed modes of variability, decadal and inter-decadal, have been found in our intermediate climate models. One mode resembles North Atlantic tri-polar sea-surface temperature (SST) patterns described elsewhere. The other mode, with mono-polar SST pattern, is novel; its key aspects include interaction of oceanic turbulence with the large-scale oceanic flow. To the extent these anomalies exist, the interpretation of observed climate variability in terms of natural and human-induced changes will be affected. Coupled mid-latitude ocean-atmosphere modes do, however, suggest some degree of predictability is possible.This research was supported by NSF
grant OCE-02-221066, DOE grants DE-FG-03-01ER63260 and
DE-FG02-02ER63413, as well as NASA grant NNG-06-AG66G-1
(MG & SK). PB has also been supported by the Newton Trust
research grant, and SK - by the University of Wisconsin-Milwaukee
Research Growth Initiative program 2006-2007
A highly nonlinear coupled mode of decadal variability in a mid-latitude ocean–atmosphere model
Author Posting. © Elsevier B.V., 2007. This is the author's version of the work. It is posted here by permission of Elsevier B.V. for personal use, not for redistribution. The definitive version was published in Dynamics of Atmospheres and Oceans 43 (2007): 123-150, doi:10.1016/j.dynatmoce.2006.08.001.This study examines mid-latitude climate variability in a model that couples turbulent
oceanic and atmospheric flows through an active oceanic mixed layer. Intrinsic
ocean dynamics of the inertial recirculation regions combines with nonlinear atmospheric
sensitivity to sea-surface temperature (SST) anomalies to play a dominant
role in the variability of the coupled system.
Intrinsic low-frequency variability arises in the model atmosphere; when run in
a stand-alone mode, it is characterized by irregular transitions between preferred
high-latitude and less frequent low-latitude zonal-flow states. When the atmosphere
is coupled to the ocean, the low-latitude state occurrences exhibit a statistically
significant signal in a broad 5–15-year band. A similar signal is found in the time
series of the model ocean’s energy in this coupled simulation. Accompanying uncoupled
ocean-only and atmosphere-only integrations are characterized by a decrease
in the decadal-band variability, relative to the coupled integration; their spectra are
indistinguishable from a red spectrum.
The time scale of the coupled interdecadal oscillation is set by the nonlinear adjustment
of the ocean’s inertial recirculations to the high-latitude and low-latitude
atmospheric forcing regimes. This adjustment involves, in turn, SST changes resulting
in long-term ocean–atmosphere heat-flux anomalies that induce the atmospheric
regime transitions.This research
was supported by NSF grant OCE-02-221066 (all co-authors) and DOE grant
DE-FG-03-01ER63260 (MG and SK)
Double Weighted Fourier Transform for the Wave Field in Inhomogeneous Medium: Some Results and Prospects
Abstract This paper discusses results of the application of double weighted Fourier transform (DWFT) to problems of communication and diagnostics of inhomogeneous media. An agreement is noted between DWFT results and results of geometrical optics, Rytov, and phase screen approximations. A relation has been found between DWFT and path integrals. Numerical simulation has been used to demonstrate the possibility of spatial signal processing based on inverse DWFT with resolution exceeding the Fresnel one during strong field fluctuations. The numerical simulation has also shown the potential applicability of this processing for reducing wave intensity fluctuations in inhomogeneous random media
The choice of the optimal approximation in the kinetic description of the vacuum creation of electron-positron plasma in strong laser fields
The paper justifies 2-similarity of kinetic equation solutions to describe vacuum emergence of electronpositron plasma under the effect of strong “laser” fields, where () is the intensity of the strong time-dependent “laser” field. The boundaries of existence of this similarity were studied
- …