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Dive into the research topics where R. M. Goody is active.

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Featured researches published by R. M. Goody.


Bulletin of the American Meteorological Society | 2002

Why monitor the climate

R. M. Goody; J. G. Anderson; Thomas R. Karl; Roberta Balstad Miller; Gerald R. North; Joanne Simpson; Graeme L. Stephens; Warren M. Washington

Abstract A successful global climate monitoring system must fulfill clear societal objectives. For some aspects of climate monitoring, the societal goals are understood and are clearly stated, but long-term, decadal/centennial climate predictions have, in the past, been judged more in terms of curiosity-led criteria. A curiosity-led climate programis not, however, the effective way to achieve the required societal objective, which is to produce thebest possible long-term climate projections. In terms of the universal use of numerical models for climateprojections, this leads to the need for monitoring programs that provide data to test model output against reliable observations. This requires an operational climate model (which the United States does not now have), and observationsthat emphasize accurate and reproducible data designed to provide critical tests of model output. The priorities for specific monitoring programs can be formulated in terms of these requirements, which can also provide metrics o...


Journal of Climate | 2005

Analysis of Sampling Errors for Climate Monitoring Satellites

Daniel Bernard Kirk-Davidoff; R. M. Goody; J. G. Anderson

Abstract Sampling retrievals of high-accuracy first-moment statistics constitute a central concern for climate research. Considered here is the important case of brightness temperature retrievals from a selection of possible orbits. Three-hourly global satellite brightness temperature data are used to predict the sampling error of monthly to annual mean brightness temperature retrieved by one or more satellites in low earth orbits. A true polar orbit is found to offer substantial advantages over a sun-synchronous orbit in the retrieval of annual mean brightness temperature, since the rotation of the local time of observation through two full diurnal cycles greatly reduces the error due to imperfect sampling of diurnal variations. Thus, a single polar orbiting satellite can produce annual mean, zonal mean brightness temperatures with typical sampling errors of less than 0.1 K, while even three sun-synchronous orbiters have high-latitude errors of up to 0.4 K. The error in retrievals of the annual mean diur...


Archive | 2010

Improve Multi-model Ensemble Climate Prediction by Using Observation Data: A Bayesian Approach

Yue Huang; Stephen Sylvain Leroy; R. M. Goody; J. G. Anderson


Archive | 2004

Promise of Climate Benchmarking Using Radio Occultation

J. G. Anderson; Stephen S. Leroy; John Andrew Dykema; R. M. Goody


Archive | 2003

Monitoring the diurnal cycle of infrared radiance from space

Daniel Bernard Kirk-Davidoff; R. M. Goody; J. G. Anderson


Archive | 2003

On-orbit SI Traceability of the Calibration of a Spectrally Resolved Measurement of Atmospheric Thermal Radiances

John Andrew Dykema; P. Jonathon Gero; R. M. Goody; J. G. Anderson


Archive | 2003

Satellite measurements of absolute spectrally resolved radiance: Benchmark climate observations to directly test climate forecast models

J. G. Anderson; R. M. Goody; John Andrew Dykema


Archive | 2002

Choosing Satellite Orbits to Minimize Sampling Error for Climate Monitoring

Daniel Bernard Kirk-Davidoff; R. M. Goody; J. G. Anderson


Archive | 2001

Satellite Instrumentation and Orbits for High Accuracy Spectrally Resolved Radiometry for Climate Monitoring

John Andrew Dykema; Daniel Bernard Kirk-Davidoff; J. G. Anderson; R. M. Goody


Archive | 1996

Ar-rhenius: A small satellite for climate research

J. G. Anderson; R. M. Goody; David W. Keith

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Graeme L. Stephens

California Institute of Technology

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Joanne Simpson

Goddard Space Flight Center

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Thomas R. Karl

National Oceanic and Atmospheric Administration

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