National Academies Press: OpenBook

Reconciling Observations of Global Temperature Change (2000)

Chapter: Appendix B: Acronyms and Abbreviations

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Suggested Citation:"Appendix B: Acronyms and Abbreviations." National Research Council. 2000. Reconciling Observations of Global Temperature Change. Washington, DC: The National Academies Press. doi: 10.17226/9755.
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Page 85

Appendix B—
Acronyms and Abbreviations

BASC

Board on Atmospheric Sciences and Climate

COADS

Comprehensive Ocean/Atmosphere Data Set

CRC

Climate Research Committee

ENSO

El Niño—Southern Oscillation

GCM

general circulation model

GHz

GigaHertz

hPa

hectoPascal

IPCC

Intergovernmental Panel on Climate Change

MSU

Microwave Sounding Unit

MSU 2LT

lower to mid-tropospheric temperature derived from MSU channel 2

NOAA

National Oceanic and Atmospheric Administration

NRC

National Research Council

RMS

root-mean-square

SST

sea surface temperature

UKMO

United Kingdom Meteorological Office

UTC

Coordinated Universal Time

WMO

World Meteorological Organization

Suggested Citation:"Appendix B: Acronyms and Abbreviations." National Research Council. 2000. Reconciling Observations of Global Temperature Change. Washington, DC: The National Academies Press. doi: 10.17226/9755.
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Suggested Citation:"Appendix B: Acronyms and Abbreviations." National Research Council. 2000. Reconciling Observations of Global Temperature Change. Washington, DC: The National Academies Press. doi: 10.17226/9755.
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Page 85
Suggested Citation:"Appendix B: Acronyms and Abbreviations." National Research Council. 2000. Reconciling Observations of Global Temperature Change. Washington, DC: The National Academies Press. doi: 10.17226/9755.
×
Page 86
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An overall increase in global-mean atmospheric temperatures is predicted to occur in response to human-induced increases in atmospheric concentrations of heat-trapping ''greenhouse gases." The most prominent of these gases, carbon dioxide, has increased in concentration by over 30% during the past 200 years, and is expected to continue to increase well into the future. Other changes in atmospheric composition complicate the picture. In particular, increases in the number of small particles (called aerosols) in the atmosphere regionally offset and mask the greenhouse effect, and stratospheric ozone depletion contributes to cooling of the upper troposphere and stratosphere.

Many in the scientific community believe that a distinctive greenhouse-warming signature is evident in surface temperature data for the past few decades. Some, however, are puzzled by the fact that satellite temperature measurements indicate little, if any, warming of the lower to mid-troposphere (the layer extending from the surface up to about 8 km) since such satellite observations first became operational in 1979. The satellite measurements appear to be substantiated by independent trend estimates for this period based on radiosonde data. Some have interpreted this apparent discrepancy between surface and upper air observations as casting doubt on the overall reliability of the surface temperature record, whereas others have concluded that the satellite data (or the algorithms that are being used to convert them into temperatures) must be erroneous. It is also conceivable that temperatures at the earth's surface and aloft have not tracked each other perfectly because they have responded differently to natural and/or human-induced climate forcing during this particular 20-year period. Whether these differing temperature trends can be reconciled has implications for assessing:

  • how much the earth has warmed during the past few decades,
  • whether observed changes are in accord with the predicted response to the buildup of greenhouse gases in the atmosphere based on model simulations, and
  • whether the existing atmospheric observing system is adequate for the purposes of monitoring global-mean temperature.

This report reassesses the apparent differences between the temperature changes recorded by satellites and the surface thermometer network on the basis of the latest available information. It also offers an informed opinion as to how the different temperature records should be interpreted, and recommends actions designed to reduce the remaining uncertainties in these measurements.

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