The Climate Change Science Program (CCSP) was the program responsible for coordinating and integrating research on global warming by U.S. government agencies from February 2002 to June 2009. [1] Toward the end of that period, CCSP issued 21 separate climate assessment reports that addressed climate observations, changes in the atmosphere, expected climate change, impacts and adaptation, and risk management issues. Shortly after President Obama took office, the program's name was changed to U.S. Global Change Research Program (USGCRP) which was also the program's name before 2002. Nevertheless, the Obama Administration generally embraced the CCSP products as sound science providing a basis for climate policy. [2] Because those reports were mostly issued after the Fourth Assessment Report of the Intergovernmental Panel on Climate Change (IPCC), and in some cases focused specifically on the United States, they were generally viewed within the United States as having an importance and scientific credibility comparable to the IPCC assessments for the first few years of the Obama Administration. [3]
The primary outputs from the CCSP were its strategic plan and 21 Synthesis and Assessment Products (SAP), five of which were released on January 16, 2009, the last business day of the Bush Administration. [4] The CCSP Strategic Plan of 2003 [5] defined five goals:
The plan also proposed 21 SAP's, each of which were designed to support one of these five goals. The plan was updated in 2008. [6] The following sections discuss the SAP's, grouped according to the five topic areas.
Three SAP's evaluated observations of climate change and our ability to definitively attribute the causes of these changes.
NOAA released the first of 21 CCSP Synthesis and Assessment reports in May 2006, entitled Temperature Trends in the Lower Atmosphere: Steps for Understanding and Reconciling Differences. [7] The report identified and corrected errors in satellite temperature measurements and other temperature observations, which increased scientific confidence in the conclusion that lower atmosphere is warming on a global scale: "There is no longer a discrepancy in the rate of global average temperature increase for the surface compared with higher levels in the atmosphere," said the report, "the observed patterns of change over the past 50 years cannot be explained by natural processes alone". [8] The report also said that "all current atmospheric data sets now show global-average warming that is similar to the surface warming. While these data are consistent with the results from climate models at the global scale, discrepancies in the tropics remain to be resolved." [7]
On January 16, 2009 (the last business day of the Bush Administration), USGS released Past Climate Variability and Change in the Arctic and at High Latitudes. [9] According to the USGS press release, [10] the report shows that:
NOAA released Re-Analyses of Historical Climate Data for Key Atmospheric Features: Implications for attribution of causes of observed change [11] in December 2008. According to the report, from 1951 to 2006 the yearly average temperature for North America increased by 1.6°Fahrenheit, with virtually all of the warmingsince 1970. During this period, the average temperature has warmed approximately 3.6 °F over Alaska, the Yukon Territories, Alberta, and Saskatchewan, but no significant warming occurred in the southern United States or eastern Canada. More than half of the warming of North America is likely (more than 66 percent chance) to have resulted from human activity.
There is less evidence that precipitation is changing. The report found no significant trend in North American precipitation since 1951, although there have been substantial changes from year to year and even decade to decade. Moreover, it is unlikely that a fundamental change has occurred in either how often or where severe droughts have occurred over the continental United States during the past half-century. Nevertheless, drought impacts have likely become more severe in recent decades. It is likely that the impacts have been more severe because the recent droughts have lasted a few years, and because warmer temperatures have created stresses in plants, which make them more vulnerable.
The US Department of Energy released the second SAP in July 2007, entitled Scenarios of Greenhouse Gas Emissions and Atmospheric Concentrations and Review of Integrated Scenario Development and Application. [12] This two-volume report explored emission scenarios that could stabilize the net effect of greenhouse gases at four different levels. It also outlined key principles and approaches for developing global change scenarios. The two reports were each written by a subset of the members of the Climate Change Science Program Product Development Advisory Committee, a panel organized under the Federal Advisory Committee Act. [13]
The report's executive summary stated that the emission reductions necessary to stabilize radiative climate forcing would "require a transformation of the global energy system, including reductions in the demand for energy... and changes in the mix of energy technologies and fuels." But the authors found great uncertainty in the price that would be necessary to stabilize climate forcing—as well as the resulting economic cost: " These differences are illustrative of some of the unavoidable uncertainties in long-term scenarios."
In addition to SAP 2.1, CCSP produced three other reports to further the goal of improving quantification of climate forcing:
As provided in the CCSP strategic plan, four SAP's examined issues under CCSP's Goal 3:
Seven SAP's examined the effects of climate change, impacts on people and natural systems, and opportunities and capacity to adapt. Those assessments provided the backbone to the Congressionally mandated Global Climate Change Impacts in the United States which was released in June 2009.
The U.S. Environmental Protection Agency released Coastal Sensitivity to Sea-Level Rise: A Focus on the Mid-Atlantic Region [21] (SAP 4.1) on January 16, 2009. According to the report's abstract, rising sea level can inundate low areas and increase flooding, coastal erosion, wetland loss, and saltwater intrusion into estuaries and freshwater aquifers. Much of the United States consists of coastal environments and landforms such as barrier islands and wetlands that will respond to sea-level rise by changing shape, size, or position. The combined effects of sea-level rise and other climate change factors such as storms may cause rapid and irreversible coastal change. Coastal communities and property owners have responded to coastal hazards by erecting shore protection structures, elevating land and buildings, or relocating inland. Accelerated sea-level rise would increase the costs and environmental impacts of these responses.
Preparing for sea-level rise can be justified in many cases, because the cost of preparing now is small compared to the cost of reacting later. Examples include wetland protection, flood insurance, long-lived infrastructure, and coastal land-use planning. Nevertheless, preparing for sea-level rise has been the exception rather than the rule. Most coastal institutions were based on the implicit assumption that sea level and shorelines are stable. Efforts to plan for sea-level rise can be thwarted by several institutional biases, including government policies that encourage coastal development, flood insurance maps that do not consider sea-level rise, federal policies that prefer shoreline armoring over soft shore protection, and lack of plans delineating which areas would be protected or not as sea level rises.
A committee set up under the Federal Advisory Committee Act monitored the progress of SAP 4.1, and questioned several aspects of the final report. The original plan included maps and estimates of wetland loss from a then-ongoing EPA mapping study conducted by James G. Titus, [22] who was also a lead author of SAP 4.1. Early drafts included the maps and results, but the final draft did not. Experts and environmental organizations objected to the deletions. The federal advisory committee also took issue with the maps' removal from SAP 4.1 and recommended that EPA publish the mapping study. [23] EPA later confirmed that EPA management had altered the report and suppressed the mapping study, although it declined to explain why. [24]
USGS released Thresholds of Climate Change in Ecosystems [25] (SAP 4.2) on January 16, 2009.
A key premise of the report was that an ecological threshold is the point at which there is an abrupt change in an ecosystem that produces large, persistent and potentially irreversible changes. The report concluded that slight changes in climate may trigger major abrupt ecosystem responses that are not easily reversible. Some of these responses, including insect outbreaks, wildfire, and forest dieback, may adversely affect people as well as ecosystems and their plants and animals. One of the greatest concerns is that once an ecological threshold is crossed, the ecosystem in question will most likely not return to its previous state. The report also emphasized that human actions may increase an ecosystem's potential for crossing ecological thresholds. For example, additional human use of water in a watershed experiencing drought could trigger basic changes in aquatic life that may not be reversible. Ecosystems that already face stressors other than climate change, will almost certainly reach their threshold for abrupt change sooner.
The United States Department of Agriculture released The Effects of Climate Change on Agriculture, Land Resources, Water Resources, and Biodiversity [26] (SAP 4.3) in May 2008. The executive summary includes the following findings.
Agriculture
Land resources
Water resources
Biodiversity
EPA released Preliminary Review of Adaptation Options for Climate-Sensitive Ecosystems and Resources [27] (SAP 4.3) in May 2008. The study focuses on national parks, national forests, national wildlife refuges, wild and scenic rivers, national estuaries, and marine protected areas, all of which are protected by the federal government. The report analyzed how to meet existing management goals set for each protected area to understand what strategies will increase the resilience of each ecosystem.
EPA concluded that climate change can increase the impact of traditional stressors (such as pollution or habitat destruction) on ecosystems, and that many existing best management practices to reduce these stressors can also be applied to reduce the impacts of climate change. For example, current efforts to reverse habitat destruction by restoring vegetation along streams also increase ecosystem resilience to climate change impacts, such as greater amounts of pollutants and sediments from more intense rainfall. EPA also concluded that the nation's ability to adapt to climate change will depend on a variety of factors including recognizing the barriers to implementing new strategies, expanding collaboration among ecosystem managers, creatively re-examining program goals and authorities, and being flexible in setting priorities and managing for change.
DOE released Effects of Climate Change on Energy Production and Use in the United States [28] (SAP 4.5) in October 2007. The report concludes that the possible impacts of climate change on energy production are important enough to start considering how to adapt. The report's executive summary summarized the report with three questions and answers:
EPA released Analyses of the Effects of Global Change on Human Health and Welfare and Human Systems. [29] (SAP 4.6) in July 2008. The report was directed by Janet L. Gamble of EPA and written by 28 authors. According to EPA, [30] some of the key conclusions of this report are:
The report was formally reviewed by an independent panel set up in compliance with the Federal Advisory Committee Act. This FACA panel's report gave a generally favorable review while providing many specific areas where improvements were needed. The advisory committee's greatest concern was that the report tried so hard to be evenhanded and not overstate what we know, that it came close to leaving the impression that we know little in cases where a lot is known. EPA revised the report to satisfy those concerns and published a response to each of the comments. [31] While not taking issue with the report's findings, the Government Accountability Project complained that EPA delayed releasing the report three months so that its results could be excluded from a regulatory finding about whether greenhouse gases threaten public health. [32]
The United States Department of Transportation released Impacts of Climate Variability and Change on Transportation Systems and Infrastructure—Gulf Coast Study [33] (SAP 4.7) in March 2008. The report was prepared by Michael Savonis of the Federal Highway Administration, Joanne Potter (a consultant to DOT), and Virginia Burkett of USGS.
The premise of SAP 4.7 was that climate is changing. Sea levels in the Gulf of Mexico are likely to rise by two to four feet over the next 50 to 100 years from the combination of climate-induced warming and land subsidence. Tropical storms are anticipated to increase in intensity and the number of heavy precipitation events is expected to increase, raising prospects of flooding and structural damage. And the number of very hot days (i.e., >90 °F) could rise by 50%.
The report concluded that the expected impacts of these climate effects on transportation are striking. A significant portion of the region's road, rail, and port network is at risk of permanent flooding if sea levels rise by four feet. This includes more than 2,400 miles (27%) of the major roads, 9% of the rail lines, and 72% of the ports. More than half (64% of interstates; 57% of arterials) of the area's major highways, almost half of the rail miles, 29 airports, and virtually all of the ports are subject to temporary flooding and damage due to increased storm intensity. The increase in daily high temperatures could increase wear on asphalt and the potential for rail buckling. Construction costs are likely to increase because of restrictions on workers on days above 90 degrees Fahrenheit.
Transportation planners can employ climate data to draw meaningful conclusions about the future. In fact, the Gulf Coast Study recommends that transportation decision makers in the Gulf Coast should begin immediately to assess climate impacts in the development of transportation investment strategies. The study also found, however, that transportation planners need new methodological tools to address the longer time frames, complexities and uncertainties that are inherent in projections of climate phenomena. Such methods are likely to be based on probability and statistics (i.e., risk assessment techniques) as much as on engineering and material science.
Three SAP's were prepared to further CCSP's Goal 5
To fulfill a statutory requirement for a national assessment, the CCSP released Scientific Assessment of the Impacts of Global Change in the United States [37] in May 2008. Shortly thereafter, a team of authors synthesized key findings from the SAP's. In June 2009, CCSP changed its name to United States Global Change Research Program and released the unified synthesis report, entitled Global Climate Change Impacts in the United States . [38] The report had ten key findings which became the bedrock of the Obama Administration's view of the impacts of climate change.
The CCSP was known as US Global Change Research Program until 2002, as authorized by the Global Change Research Act of 1990. The Bush Administration changed its name to Climate Change Science Program as part of its U.S. Climate Change Research Initiative. The Administration envisioned "a nation and the global community empowered with the science-based knowledge to manage the risks and opportunities of change in the climate and related environmental systems". President Bush reestablished priorities for climate change research to focus on scientific information that can be developed within 2 to 5 years to assist evaluation of strategies to address global change risks. [39] One the CCSP's cornerstones was the creation of 21 Synthesis and Assessment Products (SAPs) [40] to provide information to help policymakers and the public make better decisions.
The following is a list of participating agencies.
The CCSP was guided by a committee of senior representatives from each of these departments and agencies, known as the CCSP Principals. The CCSP was also overseen by the Interagency Working Group on Climate Change Science and Technology. [41] (The committee of CCSP Principals was essentially synonymous with the Subcommittee on Global Change Research of the Committee on Environment and Natural Resources under the National Science and Technology Council in the White House Office of Science and Technology Policy.) Specific program activities were coordinated through Interagency Working Groups. A coordination office facilitated the activities of the Principals and IWGs. That office as well as the IWG's continued to operate when the CCSP became the USGCRP.
The Climate Change Science Program operated during an administration that believed that continued scientific investigation was necessary before policies should be implemented.[ citation needed ] The CCSP faced the challenge of navigating the narrow path between administration officials who were sceptical of the general scientific consensus about greenhouse gases, [46] and scientific critics who were skeptical about almost everything[ clarification needed ] that the administration did related to climate change. [47] As a result, the CCSP was under more scrutiny than most federal scientific coordination programs.
The National Research Council (NRC) reviewed CCSP several times. The NRC's 2004 review [48] concluded that "the Strategic Plan for the U.S. Climate Change Science Program articulates a guiding vision, is appropriately ambitious, and is broad in scope" and "the CCSP should implement the activities described in the strategic plan with urgency." The NRC also recommended that CCSP should expand its traditional focus on atmospheric sciences to better understand the impacts, adaptation, and the human dimension of climate change. More focus on helping decision makers was necessary, it concluded.
A 2007 NRC review [49] was more critical. "Discovery science and understanding of the climate system are proceeding well, but use of that knowledge to support decision making and to manage risks and opportunities of climate change is proceeding slowly." The NRC was particularly critical of the program's failure to engage stakeholders or advance scientific understanding of the impacts of climate change on human well-being. Looking to the future of the program, a 2008 NRC report [50] put forward a set of research recommendations very similar to that embodied in the CCSP Strategic Plan revision of 2008.
The Climate Change Scientific Program was occasionally criticized for the alleged suppression of scientific information. In March 2005, Rick S. Piltz resigned from CCSP charging political interference with scientific reports: "I believe ...that the administration ... has acted to impede forthright communication of the state of climate science and its implications for society." Piltz charged that the Bush Administration had suppressed the previous National Assessment on Climate Change, by systematically deleting references to the report from government scientific documents. [51] Piltz later complained about political tinkering with the timing of SAP 4.6, [32] and suppression of sea level rise mapping studies associated with SAP 4.1. [52]
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Climate Change 2007, the Fourth Assessment Report (AR4) of the United Nations Intergovernmental Panel on Climate Change (IPCC), was published in 2007 and is the fourth in a series of reports intended to assess scientific, technical and socio-economic information concerning climate change, its potential effects, and options for adaptation and mitigation. The report is the largest and most detailed summary of the climate change situation ever undertaken, produced by thousands of authors, editors, and reviewers from dozens of countries, citing over 6,000 peer-reviewed scientific studies. People from over 130 countries contributed to the IPCC Fourth Assessment Report, which took six years to produce. Contributors to AR4 included more than 2,500 scientific expert reviewers, more than 800 contributing authors, and more than 450 lead authors.
Climate change in the US state of Washington is a subject of study and projection today. The major impacts of climate change in Washington State include increase in carbon dioxide levels, increase in temperatures, earlier annual snow melt, sea level rise, and others.
Climate change has led to the United States warming by 2.6 °F since 1970. The climate of the United States is shifting in ways that are widespread and varied between regions. From 2010 to 2019, the United States experienced its hottest decade on record. Extreme weather events, invasive species, floods and droughts are increasing. Climate change's impacts on tropical cyclones and sea level rise also affect regions of the country.
Fisheries are affected by climate change in many ways: marine aquatic ecosystems are being affected by rising ocean temperatures, ocean acidification and ocean deoxygenation, while freshwater ecosystems are being impacted by changes in water temperature, water flow, and fish habitat loss. These effects vary in the context of each fishery. Climate change is modifying fish distributions and the productivity of marine and freshwater species. Climate change is expected to lead to significant changes in the availability and trade of fish products. The geopolitical and economic consequences will be significant, especially for the countries most dependent on the sector. The biggest decreases in maximum catch potential can be expected in the tropics, mostly in the South Pacific regions.
There are many effects of climate change on oceans. One of the main ones is an increase in ocean temperatures. More frequent marine heatwaves are linked to this. The rising temperature contributes to a rise in sea levels due to melting ice sheets. Other effects on oceans include sea ice decline, reducing pH values and oxygen levels, as well as increased ocean stratification. All this can lead to changes of ocean currents, for example a weakening of the Atlantic meridional overturning circulation (AMOC). The main root cause of these changes are the emissions of greenhouse gases from human activities, mainly burning of fossil fuels. Carbon dioxide and methane are examples of greenhouse gases. The additional greenhouse effect leads to ocean warming because the ocean takes up most of the additional heat in the climate system. The ocean also absorbs some of the extra carbon dioxide that is in the atmosphere. This causes the pH value of the seawater to drop. Scientists estimate that the ocean absorbs about 25% of all human-caused CO2 emissions.
The effects of climate change on small island countries are affecting people in coastal areas through sea level rise, increasing heavy rain events, tropical cyclones and storm surges. These effects of climate change threaten the existence of many island countries, their peoples and cultures. They also alter ecosystems and natural environments in those countries. Small island developing states (SIDS) are a heterogenous group of countries but many of them are particularly at risk to climate change. Those countries have been quite vocal in calling attention to the challenges they face from climate change. For example, the Maldives and nations of the Caribbean and Pacific Islands are already experiencing considerable impacts of climate change. It is critical for them to implement climate change adaptation measures fast.
Climate change in Connecticut encompasses the effects of climate change, attributed to man-made increases in atmospheric carbon dioxide, in the U.S. state of Connecticut.
Climate change in Delaware encompasses the effects of climate change, attributed to man-made increases in atmospheric carbon dioxide, in the U.S. state of Delaware.
Climate change in Louisiana encompasses the effects of climate change, attributed to man-made increases in atmospheric carbon dioxide, in the U.S. state of Louisiana.
Climate change in Rhode Island encompasses the effects of climate change, attributed to man-made increases in atmospheric carbon dioxide, in the U.S. state of Rhode Island.
Climate change in Tennessee encompasses the effects of climate change, attributed to man-made increases in atmospheric carbon dioxide, in the U.S. state of Tennessee.
Climate change in Virginia encompasses the effects of climate change, attributed to man-made increases in atmospheric carbon dioxide, in the U.S. state of Virginia.
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Climate change in New York encompasses the effects of climate change, attributed to man-made increases in atmospheric greenhouse gases, in the U.S. state of New York. It is of concern due to its impact on the people, ecosystem, and economy of the state. Many parts of the state are already experiencing weather changes, and sea-level rise, and threatening local communities.
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