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Dive into the research topics where Stephen J. Lord is active.

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Featured researches published by Stephen J. Lord.


Bulletin of the American Meteorological Society | 2010

The NCEP Climate Forecast System Reanalysis

Suranjana Saha; Shrinivas Moorthi; Hua-Lu Pan; Xingren Wu; Jiande Wang; Sudhir Nadiga; Patrick Tripp; Robert Kistler; John S. Woollen; David Behringer; Haixia Liu; Diane Stokes; Robert Grumbine; George Gayno; Jun Wang; Yu-Tai Hou; Hui-Ya Chuang; Hann-Ming H. Juang; Joe Sela; Mark Iredell; Russ Treadon; Daryl T. Kleist; Paul Van Delst; Dennis Keyser; John Derber; Michael B. Ek; Jesse Meng; Helin Wei; Rongqian Yang; Stephen J. Lord

The NCEP Climate Forecast System Reanalysis (CFSR) was completed for the 31-yr period from 1979 to 2009, in January 2010. The CFSR was designed and executed as a global, high-resolution coupled atmosphere–ocean–land surface–sea ice system to provide the best estimate of the state of these coupled domains over this period. The current CFSR will be extended as an operational, real-time product into the future. New features of the CFSR include 1) coupling of the atmosphere and ocean during the generation of the 6-h guess field, 2) an interactive sea ice model, and 3) assimilation of satellite radiances by the Gridpoint Statistical Interpolation (GSI) scheme over the entire period. The CFSR global atmosphere resolution is ~38 km (T382) with 64 levels extending from the surface to 0.26 hPa. The global oceans latitudinal spacing is 0.25° at the equator, extending to a global 0.5° beyond the tropics, with 40 levels to a depth of 4737 m. The global land surface model has four soil levels and the global sea ice m...


Journal of Climate | 2006

The NCEP Climate Forecast System

Suranjana Saha; Sudhir Nadiga; C. Thiaw; Julian X. L. Wang; Wanqiu Wang; Qi Ming Zhang; H. M. van den Dool; Hua-Lu Pan; Shrinivas Moorthi; David Behringer; Diane Stokes; Malaquias Peña; Stephen J. Lord; Glenn Hazen White; Wesley Ebisuzaki; Pin-Yin Peng; Pingping Xie

Abstract The Climate Forecast System (CFS), the fully coupled ocean–land–atmosphere dynamical seasonal prediction system, which became operational at NCEP in August 2004, is described and evaluated in this paper. The CFS provides important advances in operational seasonal prediction on a number of fronts. For the first time in the history of U.S. operational seasonal prediction, a dynamical modeling system has demonstrated a level of skill in forecasting U.S. surface temperature and precipitation that is comparable to the skill of the statistical methods used by the NCEP Climate Prediction Center (CPC). This represents a significant improvement over the previous dynamical modeling system used at NCEP. Furthermore, the skill provided by the CFS spatially and temporally complements the skill provided by the statistical tools. The availability of a dynamical modeling tool with demonstrated skill should result in overall improvement in the operational seasonal forecasts produced by CPC. The atmospheric compon...


Weather and Forecasting | 2009

Introduction of the GSI into the NCEP Global Data Assimilation System

Daryl T. Kleist; David F. Parrish; John Derber; Russ Treadon; Wan-Shu Wu; Stephen J. Lord

Abstract At the National Centers for Environmental Prediction (NCEP), a new three-dimensional variational data assimilation (3DVAR) analysis system was implemented into the operational Global Data Assimilation System (GDAS) on 1 May 2007. The new analysis system, the Gridpoint Statistical Interpolation (GSI), replaced the Spectral Statistical Interpolation (SSI) 3DVAR system, which had been operational since 1991. The GSI was developed at the Environmental Modeling Center at NCEP as part of an effort to create a more unified, robust, and efficient analysis scheme. The key aspect of the GSI is that it formulates the analysis in model grid space, which allows for more flexibility in the application of the background error covariances and makes it straightforward for a single analysis system to be used across a broad range of applications, including both global and regional modeling systems and domains. Due to the constraints of working with an operational system, the final GDAS package included many changes...


Weather and Forecasting | 1991

The New Global Operational Analysis System at the National Meteorological Center

John Derber; David F. Parrish; Stephen J. Lord

Abstract At the National Meteorological Center (NMC), a new analysis system was implemented into the operational Global Data Assimilation System on 25 June 1991. This analysis system is referred to as Spectral Statistical Interpolation (SSI) because the spectral coefficients used in the NMC spectral model are analyzed directly using the same basic equations as statistical (optimum) interpolation. The major differences between the SSI analysis system and the conventional optimum interpolation (OI) analysis system previously used operationally at NMC are: –The analysis variables are closely related to the coefficients of the NMC spectral model. –Temperature observations are used, not heights as in the previous procedure. As a result, aircraft temperatures are being used for the first time at NMC. –Nonstandard observations, such as satellite estimates of total precipitable water and ocean-surface wind speeds, can be easily included. –No data selection is necessary. All observations are used simultaneously. –...


Bulletin of the American Meteorological Society | 2006

Improving Global Analysis and Forecasting with AIRS

J. Le Marshall; James A. Jung; John Derber; Moustafa T. Chahine; R. Treadon; Stephen J. Lord; Mitch Goldberg; Walter Wolf; Hanlan Liu; Joanna Joiner; John S. Woollen; R. Todling; P. Van Delst; Y. Tahara

AMERICAN METEOROLOGICAL SOCIETY | 891 AFFILIATIONS : LE MARSHALL, JUNG, DERBER, TREADON, LORD, GOLDBERG, WOLF, LIU, JOINER, WOOLLEN, TODLING, VAN DELST, AND TAHARA—NASA, NOAA, and U.S. Department of Defense Joint Center for Satellite Data Assimilation, Camp Springs, Maryland; CHAHINE—NASA Jet Propulsion Laboratory, Pasadena, California CORRESPONDING AUTHOR: John Le Marshall, Joint Center for Satellite Data Assimilation, NOAA Science Center, 5200 Auth Road, Camp Springs, MD 20746 E-mail: [email protected]


Monthly Weather Review | 1993

The Kinematic Structure of Hurricane Gloria (1985) Determined from Nested Analyses of Dropwindsonde and Doppler Radar Data

James L. Franklin; Stephen J. Lord; Steven E. Feuer; Frank D. Marks

Abstract A set of three-dimensional, filtered, multiply nested objective analyses has been completed for the wind field of Hurricane Gloria for 0000 UTC 25 September 1985. At this time Gloria was one of the most intense hurricanes ever observed in the Atlantic basin, with a minimum sea level pressure of 919 mb. The nested analyses, based on observations from airborne Doppler radar and Omega dropwindsondes, simultaneously describe eyewall and synoptic-scale features, and are the most comprehensive analyses of a single hurricane constructed to date. The analyses have been used to document the multiscale kinematic structure of Gloria and to investigate the relationship between the kinematic fields and the motion of the vortex. The analyses indicate that the vortex was unusually barotropic. The radius of maximum wind (RMW) was nearly vertical below 500 mb, with a slight inward slope with height between 750 and 550 mb. The strongest azimuthal mean tangential winds were found well above the boundary layer, near...


Bulletin of the American Meteorological Society | 1996

The impact of Omega dropwindsondes on operational hurricane track forecast models

Robert W. Burpee; James L. Franklin; Stephen J. Lord; Robert E. Tuleya; Sim D. Aberson

Abstract Since 1982, the Hurricane Research Division (HRD) has conducted a series of experiments with research aircraft to enhance the number of observations in the environment and the core of hurricanes threatening the United States. During these experiments, the National Oceanic and Atmospheric Administration WP-3D aircraft crews release Omega dropwindsondes (ODWs) at 15–20-min intervals along the flight track to obtain profiles of wind, temperature, and humidity between flight level and the sea surface. Data from the ODWs are transmitted back to the aircraft and then sent via satellite to the Tropical Prediction Center and the National Centers for Environmental Prediction (NCEP), where the observations become part of the operational database. This paper tests the hypothesis that additional observations improve the objective track forecast models that provide operational guidance to the hurricane forecasters. The testing evaluates differences in forecast tracks from models run with and without the ODW d...


Monthly Weather Review | 2006

Evaluation of the NCEP Global Forecast System at the ARM SGP Site

Fanglin Yang; Hua Lu Pan; Steven K. Krueger; Shrinivas Moorthi; Stephen J. Lord

Abstract This study evaluates the performance of the National Centers for Environmental Prediction Global Forecast System (GFS) against observations made by the U.S. Department of Energy Atmospheric Radiation Measurement (ARM) Program at the southern Great Plains site for the years 2001–04. The spatial and temporal scales of the observations are examined to search for an optimum approach for comparing grid-mean model forecasts with single-point observations. A single-column model (SCM) based upon the GFS was also used to aid in understanding certain forecast errors. The investigation is focused on the surface energy fluxes and clouds. Results show that the overall performance of the GFS model has been improving, although certain forecast errors remain. The model overestimated the daily maximum latent heat flux by 76 W m−2 and the daily maximum surface downward solar flux by 44 W m−2, and underestimated the daily maximum sensible heat flux by 44 W m−2. The model’s surface energy balance was reached by a ca...


Bulletin of the American Meteorological Society | 1998

Maturity of Operational Numerical Weather Prediction: Medium Range

Eugenia Kalnay; Stephen J. Lord; Ronald D. McPherson

Abstract In 1939 Rossby demonstrated the usefulness of the linearized perturbation of the equations of motion for weather prediction and thus made possible the first successful numerical forecasts of the weather by Charney et al. In 1951 Charney wrote a paper on the science of numerical weather prediction (NWP), where he predicted with remarkable vision how NWP would evolve until the present. In the 1960s Lorenz discovered that the chaotic nature of the atmosphere imposes a finite limit of about two weeks to weather predictability. At that time this fundamental discovery was “only of academic interest” and not really relevant to operational weather forecasting, since at that time the accuracy of even a 2-day forecast was rather poor. Since then, however, computer-based forecasts have improved so much that Lorenzs limit of predictability is starting to become attainable in practice, especially with ensemble forecasting, and the predictabilty of longer-lasting phenomena such as El Nino is beginning to be ...


Monthly Weather Review | 1992

A Nested Spectral Model for Hurricane Track Forecasting

Mark DeMaria; Sim D. Aberson; Katsuyuki V. Ooyama; Stephen J. Lord

Abstract A numerical method for analysing and forecasting a wide range of horizontal scales of motion is tested in a barotropic hurricane track forecast model. The numerical method uses cubic B-spline representations of variables on nested domains. The spline representation is used for the objective analysis of observations and the solution of the prediction equations (shallow-water equations on a Mercator projection). This analysis and forecasting system is referred to as VICBAR (Vic Ooyama barotropic model). The VICBAR model was tested in near real time during the 1989 and 1990 Atlantic hurricane seasons. For the 1989 season, VICBAR had skill comparable to, or greater than, that of the operational track forecast models. For the, 1990 season, VICBAR had skill comparable to that of the operational track-forecast models. During both 1989 and 1990, VICBAR had considerably more skill for forecasts of hurricanes than for forecasts of tropical storms. For the 1990 season, VICBAR was generalized to include time...

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John Derber

Cooperative Institute for Meteorological Satellite Studies

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John S. Woollen

Science Applications International Corporation

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James L. Franklin

National Oceanic and Atmospheric Administration

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Russ Treadon

National Oceanic and Atmospheric Administration

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Zoltan Toth

National Oceanic and Atmospheric Administration

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Shrinivas Moorthi

National Oceanic and Atmospheric Administration

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David Behringer

National Oceanic and Atmospheric Administration

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Frank D. Marks

National Oceanic and Atmospheric Administration

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James A. Jung

Cooperative Institute for Meteorological Satellite Studies

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