In December 1997 in Kyoto, Japan, the community of nations reached a historic agreement to collectively curb the growth of carbon dioxide and other radiatively active gases in the atmosphere. The intense 1997–1998 El Niño, although not necessarily related to the carbon dioxide increase, made clear the importance of climate variations. The event caused anomalous weather, some of it beneficial (fewer hurricanes in the Atlantic), but much of it adverse (record rainfall in the western and southern portions of the United States and drought in Indonesia). Agriculture, ecosystems, water supply systems, and public health are potentially vulnerable to natural variability and changes in climate. The leaders of the developed and developing nations recognize that climate changes are likely to have significant impacts on their economies, foreign policies, and quality of life in the coming decades.
The 1997 Conference on the World Climate Research Programme to the Third Conference of the Parties of the United Nations Framework Convention on Climate Change concluded that the global capacity to observe the Earth's climate system is inadequate and is deteriorating worldwide: ''Without action to reverse this decline and develop the Global Climate Observation System, the ability to characterize climate change and variations over the next 25 years will be even less than during the past quarter century" (See Appendix A). As a result, the chair of the subcommittee of the U.S. Global Change Research Program (USGCRP) requested a National Research Council study to assess the current status of the climate observing capabilities of the United States. This report focuses on existing observing systems for detection and attribution of climate change, with special emphasis on those systems with long time series.
As will be shown in this report, these systems require immediate action to reverse their decay and to redesign them.
Climate impacts most economic sectors, including energy, food and fiber, transportation, human health, biological resources, and living conditions. These activities are influenced by precipitation and water availability, temperature, storms, solar radiation, and sea level, and how they vary over time and with geography. Variables most useful for climate change detection and attribution are: three-dimensional temperature and water vapor; surface wind, sea level pressure, precipitation; sea ice and ice sheet properties; streamflow, groundwater and land water reservoirs; vegetation cover; and ocean upper-level temperature and salinity, deep ocean temperature and salinity profiles and the height of sea level.
Most observing systems that monitor climate were established to provide data for defined purposes, such as predicting daily weather; advising farmers; warning of hurricanes, tornadoes and floods; managing water resources; aiding ocean and air transportation; and understanding the role of the ocean in climate change. Many federal and state agencies, including the Departments of Agriculture, Commerce, Defense, and Interior, and NASA, collect these data. In some departments, several agencies operate observing systems. For example, in Defense, the Air Force, Navy, and Corps of Engineers operate networks that observe some of these variables.
The purpose of these observations continues to evolve with changes in mission, with the development of new technologies, and more recently with restrictions on budgets. The priorities to maintain the observation networks vary widely from agency to agency. In general, management of the programs has not recognized the importance of the observations for detection and attribution of climate change. The departments and agencies should strengthen and revitalize the partnerships that generated long-term records of many of these variables.
Climate researchers have used existing, operational networks because they have been the best, and sometimes only, source of data available. They have succeeded in establishing basic trends of several aspects of climate on regional and global scales. Deficiencies in the accuracy, quality, and continuity of the records, however, still place serious limitations on the confidence that can be placed in the research results. Federal agencies should undertake a joint effort to improve the observations from these networks.
The panel concludes that the ten climate monitoring principles proposed by Karl et al., 1995, should be applied to climate monitoring systems:
The panel's evaluation of existing climate records, using these ten principles, shows that only about half of the principles are being followed for some of the variables most useful for climate change detection and attribution. For other records, only one or two principles are being followed adequately. The application of all but one of the principles of climate monitoring needs improvement.
If federal agencies are to serve society's needs for well-informed climate decisions, they should strive to preserve the value of the past climate record and to build improved and more valuable climate records in the future. Although this report focuses on existing observational systems, especially those with long data records, it is important to stress that this represents only a part of the needs for climate data. Programs to develop new records also should be undertaken, and should take advantage of such new technology as geostationary and polar orbiting satellites.
A word of caution, however: for many years, satellite remote sensing has been suggested as the answer to climate monitoring. Indeed, the growing emphasis on operational mesoscale weather observing and forecasting initiatives inevitably will lead to a growing reliance on remote sensing—both surface- and space-based. If, in the process, in situ networks such as the radiosonde are reduced in size or importance, there could be a large negative impact on the ability to assess climate and climate change. The panel recognizes that many of the atmospheric observations in ocean areas can be provided only by global systems such as satellites. At the moment, however, there is only sketchy information on the suitability of remotely sensed data as a source for climate change detection and attribution. Some studies have shown a positive impact of
these data. Others have clearly indicated substantial problems, two of which are calibration and poorly documented changes in the instrument performance from one satellite to the next.
FINDING: There has been a lack of progress by the federal agencies responsible for climate observing systems, individually and collectively, toward developing and maintaining a credible integrated climate observing system, consequently limiting the ability to document adequately climate change.
RECOMMENDATION: These agencies should work through the USGCRP process and at higher government levels to:
In the near term, the USGCRP agencies can ameliorate this situation by taking the following actions: