Optimization Of Multiclass Queueing Networks With - Changeover Times Via(Correct)
1992)In a companion paper (see Bertsimas and Nino-Mora 1999) we address the corresponding problem in
First Type Represents Palm 308 D. Bertsimas And J. Nino-Mora Moments Of Queue Lengths With Respect To
(1995)using potential function techniques, and in Nino-Mora (1995)using the flow conservation halweb.uc3m.es/jnino/eng/pubs/mqn1.pdf
Tracking down the ENSO delayed oscillator - With An Adjoint(Correct)
runs are reported, tracing the sensitivities of the NINO3 and NINO3.4 indices in October 1987, December
tracing the sensitivities of the NINO3 and NINO3.4 indices in October 1987, December 1987 and
be related to a single function, for example, the NINO3 index of sea surface temperature in the eastern www.knmi.nl/onderzk/oceano/publ/oldenbor/oldenbor01.ps.gz
A Linear Stochastic Dynamical Model of ENSO. Part II: Analysis - Thompson And Battisti(Correct)
ENSO, and at achieving some skill in predicting El Nino events. This success started with the Zebiak and
was scaled so that the average variance of the Nino-3 index (SSTA average in the area 58N-58S, and
from the simulation would match the average Nino-3 variance of the Comprehensive Ocean-Atmosphere www.atmos.washington.edu/~david/tb3.ps
Nonlinear multichannel singular spectrum analysis of the.. - William Hsieh And(Correct)
Than The Cool Periods, As Observed For The El Nino-Southern Oscillation. Also In The Ssta Nlssa Mode
the SSTA data. As we want to resolve the ENSO (El Nino-Southern Oscillation) variability, a window 7 of
full La Nina cool events (Fig. 4c)ii) The El Nino warm events are strongest near the eastern www.ocgy.ubc.ca/~william/Pubs/NLSSA.jgro.ps
Computing Stationary Probability Distributions and Large.. - Gamarnik (2002)(Correct)
[2]and using more direct methods, Bertsimas and Nino-Mora [3]4] All of the results obtain only
(2001)no. 4, 1384-1428. 3] D. Bertsimas and J. Nino-Mora, Optimization of multiclass queueing networks www.research.ibm.com/people/g/gamarnik/Papers/StationaryProbUndec.ps
Indonesian wildfires of 1997: Impact on tropospheric chemistry - Duncan Bey Chin (2003)(Correct)
year-long drought induced by the most extreme El Nino-Southern Oscillation (ENSO) event of the century
W. Min, and W. G. Read, Effects of 1997 -1998 El Nino on tropospheric ozone and water vapor, Geophys.
Glantz, M. H.Currents of Change:Impacts of El Nino and La Nina on Climate and Society, pp. 84 -100, www-as.harvard.edu/chemistry/trop/publications/duncan2003.pdf
Variational Assimilation of TAO and XBT Data in the.. - Bonekamp, van.. (2001)(Correct)
[1999] monitored the evolution of the strong El Nino of 1997/1998 down to an ocean depth of 500 meter.
of data assimilation on ocean initialization and El Nino prediction, Mon. Weath. Rev.125, 742-753,
M. J.Genesis and evolution of the 1997-98 El Nino, Science, 283, 950-954, 1999. McPhaden, M. J. www.knmi.nl/onderzk/oceano/publ/oldenbor/vardams1.ps.gz