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Updated 3 December 2007

Land Use / Land Cover Change
USGCRP Fiscal Years 2004-2005 Accomplishments

 

USGCRP
Program Elements

Atmospheric Composition

Ecosystems

Global Carbon Cycle

Decision-Support Resources Development and Related Research on Human Contributions and Responses

Climate Variability and Change

The Global
Water Cycle

Observing and Monitoring the Climate System

Communications

International Research and Cooperation

 

The following are selected highlights of recent research supported by CCSP participating agencies (as reported in the fiscal year 2006 edition of the annual report, Our Changing Planet).

 

Projecting Area Changes for Major Forest Types [1]

Modeling the dynamics of forest cover changes is part of the periodic national forest resource assessments by the USDA Forest Service and cooperators. One of the largest changes in U.S. forest type areas over the last half-century has involved pine forest types in the South. The area of planted pine has increased more than 10-fold since 1950, mostly on private lands. Baseline projections indicate a net increase of about 5.6 million ha (about 13.8 million acres), which is approximately a 52% increase in planted pine area in the South over the next 50 years. This forest investment is expected to result in a significant increase in sequestered carbon per acre. With increasing amounts of timber harvests arising from plantations, this will also affect carbon storage in wood products. U.S. forests elsewhere will also continue to change in structure and composition, as the area of timberland with trees older than 150 years on National Forest lands is projected to more than double by 2050. Many of those forests are in the Pacific Northwest and can lead to a notable increase in sequestered forest carbon.

Population, Land Use, and Climate Change Impacts on Regional and Local Water Supply and Demand [12]

Forest Service scientists assessed the effects of model-projected climate change scenarios coupled with potential changes in population, hydrology, and land use/land cover to examine future water supply and demand across the southern United States. Long-term average, maximum, and minimum water yield and demand were examined. Water yield reflects the combined influences of vegetation, soils, precipitation, temperature, and evaporation. The study found that current water yield exceeds water demand by more than 100 times during an average precipitation year in the region. However, some local areas are currently experiencing significant water shortages due to high population density, water demand, and/or periodic drought. Overall, the climate projections suggest that total water yield will increase in the region over the next 20 years. Local water shortages are projected to increase and expand in area during the next 20 years, with population change having the greatest impact on local water supply stress. Projected changes in climate and vegetative cover will have larger region-wide impacts on water yield, but relatively little impact on local changes in water supply stress compared to population change (see Figure 13).

Figure 13: Percentage Change in Water Stress

Figure 13: Percentage Change in Water Stress. Projection of effects of changes in population and climate on changes in water stress between 1990 and 2025. This projection used the Hadley 2 Climate Model with sulfates included to project precipitation and air temperature out to 2025; U.S. census demographic projections to 2025; and 1992 Multi-Resolution Land Characteristics (MRLC) vegetation data. Credit: S. McNulty, USDA/Forest Service.

Lowland Forest Loss in Protected Areas of Indonesian Borneo [3]

Analysis of lowland forest loss in protected areas of Indonesian Borneo ( Kalimantan) demonstrates progress toward understanding how complex histories of land use, land cover, policy, and sudden economic change can result in rapid change in land cover. These findings will contribute to improved ecosystem modeling. Satellite remote sensing of land-cover change between 1985 and 2001 reveals rapid and pervasive deforestation of lowland forests within protected areas: a 56% loss (>29,000 km2 ) was documented across Kalimantan. Socioeconomic and political drivers of these land-use changes were examined for the period 1970 to 2002. The collapse of logging concession timber stocks through overexploitation, coupled with high demand for timber by wood-based industries and policies that promote oil palm plantations, drive both illegal logging and forest clearing. In combination, these land-use changes result in lowland forest fragmentation and loss of wildlife habitat (see Figure 14).

Results of this research are being applied to verify forest inventories, update estimates of tropical carbon emissions dynamics, and assess effects on biodiversity. In Indonesia, these products are being used by nongovernmental organizations, multilateral donors, and governmental agencies to increase transparency, accountability, and management in remote frontier areas with the aim of reducing illegal logging.

Figure 14: Forest Clearing in Gunung Palung National Park, 1988–2002

Figure 14: Forest Clearing in Gunung Palung National Park, 1988–2002. Cumulative forest loss within the Gunung Palung National Park boundary (yellow line), Indonesia, and its surrounding 10-km buffer. Forest and non-forest classifications are based on Landsat Thematic Mapper time series. Lowland (green) and peat (olive) forests were converted to non-forest (red), first predominantly in the buffer and later within the park. Grey areas are montane forest and excluded from the analyses. Credit: S.N. Trigg, University of Maryland (from Curran et al., 2004).

Simulating Urban Development in the Baltimore-Washington, D.C., Area [2 , 7, 11]

Using an existing urban model, scientists simulated patterns of urban development in the Baltimore-Washington, D.C., area. Empirical calibration of the model using Landsat Thematic Mapper image maps of past change between 1986 and 2000 provided calibration of the model using fine-scale data, and refined model projections of future change. The data set also enabled an extensive sensitivity analysis of the model. To serve regional planning needs, the multi-agency Chesapeake Bay Program is now supporting the creation of 30-year projections for the entire Bay watershed that will inform vulnerability assessments and decision support. These scenarios range from one that assumes a continuation of current growth trends and environmental protection policies, to one that assumes stronger environmental protection on open lands and greater use of mass transit. This research is at the forefront of urban modeling, creating fine-scale projections over large areas, using methods grounded in urban theory and economics, and incorporating satellite remote-sensing products (see Figure 15).

Figure 15: Percentage of Development Patterns in 2030

Figure 15: Percentage of Development Patterns in 2030. Using a cell-based urban model (SLEUTH), projections of development patterns in 2030 were created assuming three different policy scenarios (current trends, managed growth, and low growth). SLEUTH was calibrated using Landsat-derived maps of the built environment that documented development patterns between 1986 and 2000. This data set provided a baseline that the calibrated model used to extrapolate patterns into the future. Following business-as-usual patterns of low density and dispersed development, this model projects that the amount of developed land could increase 123%, putting at least 1,300 km2 of forests and 1,537 km2 of agricultural lands at risk.   Credit: C. Jantz and S. Goetz,  The Woods Hole Research Center.

Impervious Surface Area Grid of the United States [6]

The construction and maintenance of impervious surfaces (buildings, roads, parking lots, roofs, etc.) constitutes a major human alteration of the land surface, changing the local hydrology, climate, and carbon cycling. The United States is adding impervious surface area at a rapid pace. Population is increasing at a rate of 3 million people per year. Annual U.S. public and private sector construction spending is greater than $480 billion. This includes more than one million new single-family homes and more than 10,000 miles of new roads per year. Given these trends, impervious surface area is likely to become a more prominent environmental and growth management issue in the coming years. However, few areas have mapped impervious surface area, due in part to the technical challenges and cost constraints of using high spatial resolution (e.g., 1-m) data for direct mapping of constructed surfaces. As an alternative, existing national coverage data sources have been used to model the percent cover of impervious surface area on a 1-km grid for the conterminous United States. The data sources included satellite-observed nighttime lights, three classes of Landsat-derived urban land cover, and U.S. Census Bureau road vectors. The results indicate that total impervious surface area of the 48 states (and D.C.) is 112,610 (±12,725) km2 , which is slightly smaller than Ohio (116,534 km2 ; see Figure 16).

Figure 16: Fractional Impervious Surface Area

Figure 16: Fractional Impervious Surface Area. The U.S.-constructed impervious surface area (ISA) in 2000 was nearly the size of Ohio. Population is increasing at a rate of 3 million people per year. Annual U.S. public and private sector construction spending is greater than US$480 billion. This includes more than a million new single-family homes and more than 10,000 miles of new roads per year. Credit: C.D. Elvidge, NOAA/National Geophysical Data Center.

Modeling Global Change Impacts on Wildfire Cycles [8]

A Geographic Information System (GIS) model (FCS-1) has been developed to enable research on how the combined impacts of climate, fire, and human activities influence the nature, distribution, and intensity of fire risk at scales relevant to management concerns and needs. FCS-1 was developed with the recognition that strategic land management requires an understanding of fire behavior and community needs over time. The model incorporates traditional fire science with the human dimension of landscape management in order to identify assets (e.g., property and recreation opportunities) at risk in case of fire. A study utilizing this model emphasized evaluation sessions involving both experts and community members. The evaluation sessions provided valuable opportunities to improve scientific understanding of (a) the ways in which models like FCS-1 might be employed in strategic planning activities to address fire risk problems, and (b) the levels of confidence held by decisionmakers, scientists, and community members in the various types of scientific information contained in the model.

Establishing the Effects of the Soviet Union's Collapse on the Onset of Spring across Kazakhstan [4, 5, 10]

Agricultural policies in centrally planned economies of the Soviet Union left enduring legacies of land-surface transformations across eastern Europe and northern Eurasia. The collectivization efforts of the 1930s and 1950s reorganized the land-patch dynamics of cultivated landscapes. The collapse of the economic and political institutions of the Soviet Union at the beginning of the 1990s led to widespread agricultural de-intensification, land abandonment, loss of livestock, and decreased grazing pressure. Mixed into the record of satellite observations of the vegetated land surface are multiple sources of variation: seasonality, interannual climatic variation, changes in observing sensors, and human activity, including land-use/ land-cover change. Methods were developed to differentiate the influences of human activities from the other sources of variation at a spatial scale appropriate to link with mesoscale meteorological models. The research focused on Kazakhstan, the ninth largest country in the world in land area, spanning both semi-arid to arid regions dominated by dryland agriculture and grazing, providing an excellent example of post-Soviet land-use/land-cover change. Of the nineteen ecoregions in Kazakhstan, twelve exhibit strong spring seasonality. Nine of those twelve have shown significant changes in growing season vegetation dynamics when comparing the 1980s under the Soviet regime with the late 1990s (see Figure 17). These change analysis methodologies are transferable to other regions dominated by temperate vegetation.

Figure 17: Significant Changes in Observed Growing Season: Kazakhstan

Figure 17: Significant Changes in Observed Growing Season: Kazakhstan. Significant changes in growing season have been detected in many of the 19 ecoregions across Kazakhstan. Credit: G. Henebry, University of Nebraska-Lincoln.

Synthesis of Land-Cover and Land-Use Research [9]

A synthesis of work carried out under the auspices of NASA's Land-Cover and Land-Use Change Program over the past 8 years was published in 2004. This program involves hundreds of scientists who have worked to understand human impacts on land cover, which is one of the most important forces changing our planet. The work reported in the volume and accompanying CD spans the natural and the social sciences, and describes the application of state-of-the-art techniques for understanding the Earth. These techniques include satellite remote sensing, geographic information systems, modeling, and advanced computing. The volume includes detailed case studies, regional analyses, and globally scaled mapping efforts.


 

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