Land use

[2]: 2914  Land-use change, together with use of fossil fuels, are the major anthropogenic sources of carbon dioxide, a dominant greenhouse gas.[2]: 2914  Land-use change, together with use of fossil fuels, are the major anthropogenic sources of carbon dioxide, a dominant greenhouse gas.[19] The reshaping of landscapes to serve human needs, such as the deforestation for farmland, can have long-term effects on earth systems and exacerbate the causes of climate change.[20] Although the burning of fossil fuels is the primary driver of present-day climate change, prior to the Industrial Revolution, deforestation and irrigation were the largest sources of human-driven greenhouse gas emissions.[20] Increasing land conversion by humans in future is not inevitable: In a discussion on response options to climate change mitigation and adaptation an IPCC special report stated that "a number of response options such as increased food productivity, dietary choices and food losses, and waste reduction, can reduce demand for land conversion, thereby potentially freeing land and creating opportunities for enhanced implementation of other response options".[25] Studying risk and vulnerability entails the development of quantitative, qualitative, and geospatial models, methods, and support tools.[26] The purpose of these tools is to communicate the vulnerability of both human communities and natural ecosystems to hazard events or long-term land change.Modeling risk and vulnerability requires analyses of community sensitivity to hazards, an understanding of geographic distributions of people and infrastructure, and accurate calculation of the probability of specific disturbances occurring.[32] This leads to the overexploitation of farmland, and down the line results in desertification, another land cover change, which renders soil unusable and unprofitable, requiring farmers to seek out untouched and unpopulated old-growth forests.[30] For example, road and railway expansions designed to increase quality of life have resulted in significant deforestation in the Amazon and Central America.[33] According to the United Nations, the global urban population has increased rapidly since 1950, from 751 million to 4.2 billion in 2018, and current trends predict this number will continue to grow.[39] However, a water diversion project, undertaken by the Soviet Union to irrigate arid plains in what is now Kazakhstan, Uzbekistan, and Turkmenistan, resulted in the Aral Sea losing 85% of its land cover and 90% of its volume.[38][39] Additionally, scientists have been able to use technology such as NASA's Moderate Resolution Imaging Spectroradiometer (MODIS) to track changes to the Aral Sea and its surrounding climate over time.As society shifted from rural to urban, public land regulation became important, especially to city governments trying to control industry, commerce, and housing within their boundaries.Judicial decisions and enforcement of private land-use arrangements can reinforce public regulation, and achieve forms and levels of control that regulatory zoning cannot.
Cumulative CO2 emissions from land-use change (as of 2021). Emissions from land-use change can be positive or negative depending on whether these changes emit (positive, brown on the map) or sequester (negative) carbon (green on the map).
A graphic description of land use in the Australian Capital Territory as of 2017. Colours represent different uses.
The development of global land use over the centuries and millennia: more and more of the world's habitable land is used for agriculture.
Global distribution of land used for agriculture
Predicting the effects of deforestation on rainfall in Brazil, an example of land change modeling.
Rainforest deforestation for land use conversion
An aerial image of New Delhi , India, one of the world's largest urban areas
Remote sensing images show changes to the extent of the Aral Sea from 1989 (left) to 2014 (right).
CO2 emissionsland managementforest landagricultural landgrasslandwetlandssettlementsimpacts on the environmenturban sprawlsoil erosionsoil degradationland degradationdesertificationnatural resourcesnutrientsplantsanimalsfossil fuelsanthropogenicgreenhouse gasdeforestationstudy of land changeland change modelingAustralian Capital TerritoryUnited NationsFood and Agriculture Organizationarable landUS Department of Agriculturecontiguous 48 statesPastureForestCroplandLand change scienceEarth systemsclimate changetemperate regionsland coverfarmlandIndustrial Revolutionirrigationgreenhouse gas emissionsagricultureclimate change mitigationadaptationIPCC special reportdietary choicesland-coversatellite imageryremotely sensed dataquantitativequalitativedisturbancesLand change modelsland-cover.resource managementnatural environmentsocio-economichuman-environment systemssustainabilitycarbon capturebiodiversityold-growth forestAmazonCentral Americaexportsforeign debtNew Delhiurbanizationecological footprintgoods and servicesurban heat island effect.Aral SeaSoviet UnionKazakhstanUzbekistanTurkmenistansalinizationModerate Resolution Imaging Spectroradiometer (MODIS)jurisdictionsland-use planningland-use conflictszoning regulationsurban growth boundaryPortland, OregonHabitat fragmentationIndiana Dunes National LakeshoreNew York Cityzoningdevelopmentstatutory lawNational Historic Preservation Act of 1966National Environmental Policy ActCultural landscapeLand use, land-use change and forestryLand-use forecastingIndirect land use change impacts of biofuelsLand-use conflictGlobal Environmental ChangeBibcodeGlobal Ecology and BiogeographyUnited Nations Convention to Combat DesertificationWorld BankBloombergVogel, ColeenScienceProceedings of the National Academy of SciencesIntergovernmental Panel on Climate ChangeWayback MachineVillage of Euclid, Ohio v. 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