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Heating up the forest: open-top chamber warming and Duke Forests
Heating up the forest: open-top chamber warming and Duke Forests

Your opinion on climate change might not be as common as you think
Your opinion on climate change might not be as common as you think

... consensus effect1 (a tendency to overestimate how common one’s ‘own’ opinion is) and pluralistic ignorance2 (where most people privately reject an opinion, but assume incorrectly that most others accept it). We investigated these biases in people’s opinions about the existence and causes of climate ...
The politics of climate change
The politics of climate change

... as there is a consensus about its extent and dangers, it has played a large part in building it. Indeed, that is its declared aim—to gather together as much scientific data as possible, subject it to rigorous review, and reach overall conclusions on the state of scientific opinion. In successive pub ...
- UNM Digital Repository
- UNM Digital Repository

... projections for a doubling of CO 2 are remarkably consistent among a number of different models. This consistency suggests a strong probability that the basic projections-namely, that a doubling of atmospheric CO 2 will cause a 2-4°C average global temperature increase, amplified to 1012'C at the No ...
- Arctic Monitoring and Assessment Programme
- Arctic Monitoring and Assessment Programme

... scenario of future warming, not a worst-case scenario. Compared to the full range of scenarios analyzed by the Intergovernmental Panel on Climate Change (IPCC), the primary scenario used in the ACIA analyses falls below the middle of the IPCC range of projected temperature rise. The results summariz ...
Consequences of Global Warming of 1.5 °C and 2 °C for Regional
Consequences of Global Warming of 1.5 °C and 2 °C for Regional

... is especially pertinent to avoid the worst impacts of rising sea levels, and declining Arctic sea ice among other factors [9]. Unlike 2˚C, the 1.5˚C target is relatively unexplored, and studies highlighting its feasibility and impacts are beginning to emerge [10–13]. Under most low emission scenario ...
PDF
PDF

... making future policy on climate change. Only 18.32% of the farmers perceived that all factors were going to be taken into consideration, while most (81.68%) were of the view that this was not going to occur. The most serious indictment of loss of trust in government emerged when the farmers’ opined ...
Climate Literacy Principles
Climate Literacy Principles

... coming season is likely to be different from climatology (see definition). Climate forecasts are generally based on the chances (or probability) that an event will occur, for example that rainfall or temperature will be either below normal, near normal, or above normal. ...
Australian Species and Climate Change - WWF
Australian Species and Climate Change - WWF

... Australia with a range stretching from the Murchison River in the north, inland to Coorow, Kellerberrin and Lake Cronin, and south to Esperance. It is classified as endangered according to the criteria of the World Conservation Union (IUCN) and Australian Government and ‘Rare or likely to become ext ...
Changes in the precipitation at Keszthely according to the
Changes in the precipitation at Keszthely according to the

Urban Heat Island and Air Quality of London, UK
Urban Heat Island and Air Quality of London, UK

... favour the creation of more temperature inversions trapping pollutants in the nearsurface layer of the atmosphere. For example, it has been estimated that a 1 degree Celsius rise in summer air temperatures (also a proxy for the amount of catalysing sunshine) is associated with a 14% increase in surf ...
PDF - Oxford Academic - Oxford University Press
PDF - Oxford Academic - Oxford University Press

... partial explanation for the existence of massive phytoplankton blooms that are observed in some polar ecosystems (Smith and Gordon, 1997). That conclusion was based on an analysis of hundreds of data points obtained for protists growing in culture, but studies that have examined the growth rates of ...
Climate variability and change: a perspective from the oceania region
Climate variability and change: a perspective from the oceania region

... to the problem of determining the forcing functions responsible for climate change. The method was applied to the change in the temperature structure of the atmosphere between the 20 year periods 1949–68 and 1975–94. The external forcing function is largely zonally symmetric, consistent with large s ...
Aalborg Universitet Heiselberg, Per Kvols
Aalborg Universitet Heiselberg, Per Kvols

... 2.2 Climate scenarios Table 2 summarizes the climate scenarios considered in this study. As references, building’s performance for the climate of Växjö are modelled ...
Changing Northern Hemisphere Storm Tracks in an Ensemble of
Changing Northern Hemisphere Storm Tracks in an Ensemble of

... While the former Intergovernmental Panel on Climate Change (IPCC) report (Houghton et al. 2001, p. 73) stated that there was little agreement among models concerning future changes in storm intensity, frequency, and variability, the IPCC AR4 (Solomon et al. 2007) mentions that “extra-tropical storm ...
Future Climate Impact on the Desertification in the Dry Land Asia
Future Climate Impact on the Desertification in the Dry Land Asia

... clear that the degradation has led to the creation of desert-like conditions [7]. Warming trends and increasing temperature extremes have been observed in most of Asia over the past century, but there is much uncertainty in future precipitation; this is critical because water scarcity is expected to ...
Marine boundary layer clouds at the heart of tropical cloud feedback
Marine boundary layer clouds at the heart of tropical cloud feedback

... of the tropical circulation, and that it is maximum in regions of strong subsidence. The reasons for that large sensitivity might be related to the breakup, as SST increases, of stratiform low-level cloud types (stratus, stratocumulus) into more cumuliform clouds (trade cumulus), and thus to a small ...
Building Place-Based Climate Change Education
Building Place-Based Climate Change Education

... ,QWKH:DVKLQJWRQ'&DUHDVSULQJÀRZHULQJRI 100 different species has advanced by 2.4 days from WR,QWKH3DFL¿F1RUWKZHVW¶V&DVFDGH Mountains, decreasing snowpack at mid-elevation stations show a 30-60 percent decline from 1950$QGVSHFLHV¶UDQJHVDUHVKLIWLQJ2YHUWKHSDVW ...
the full ITEP workshop booklet
the full ITEP workshop booklet

... Using  environmental  sensors  often  require  the  use  of  maps  in  order  to  make  sense  of   sensor  data.  Mapping  is  also  a  gateway  to  thinking  about  how  climate  change  can  influence   a  community.  Useful  maps ...
An overview of climate change impacts on European viticulture
An overview of climate change impacts on European viticulture

... content, and yield. Other berry organoleptic properties such as color, flavor, and aroma components are inhibited by excessive solar radiance and severe dryness too. This results in unbalanced wines, with high alcoholic content and excessively low acidity (Jones 2004). In this context, the Mediterra ...
Response of river flow regime to various climate change scenarios
Response of river flow regime to various climate change scenarios

... Meghna River, being a major drainage outlet of the basin, is likely to be affected by such variability and hence its response to climate can be studied through the use of plausible scenarios of climate change. In this study, an artificial neural network (ANN) model, based on future climate projectio ...
Climate notes
Climate notes

... • Even short-term changes in the climate may lead to long-lasting effects that may make the survival of life on Earth more difficult for both humans and other species. • Some of these potential climate changes include global warming, sea-level changes, and changes in precipitation. Chapter menu ...
Climate Change and International Relations Theory: Northeast Asia as a Case Study
Climate Change and International Relations Theory: Northeast Asia as a Case Study

... Hydrology and Water Sources The climate change-altered hydrological cycle in Northeast Asia is already making the East Asian monsoon more variable and increasing the frequency and magnitude of both extreme precipitation and drought events. More frequent heatwave conditions are likely across the regi ...
MS TAIMUN I Chair Reports Committee: Environment Committee
MS TAIMUN I Chair Reports Committee: Environment Committee

... Bangladesh: Bangladesh, with its southern region vulnerable to floods, fear the monsoons. Cambodia: Like its neighbors, Thailand and Bangladesh, Cambodia’s southwestern region is exposed to the sea. China: The entire East, South, and South-eastern regions of the massive nation are all vulnerable to ...
The geography of climate change: implications
The geography of climate change: implications

... The use of climate and species modelling to inform conservation faces (at least) two fundamental challenges. First, different species are expected to exhibit distinct, individualistic responses. Even if it were possible to accurately project climate change and to precisely model the biological respo ...
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Effects of global warming



The effects of global warming are the environmental and social changes caused (directly or indirectly) by human emissions of greenhouse gases. There is a scientific consensus that climate change is occurring, and that human activities are the primary driver. Many impacts of climate change have already been observed, including glacier retreat, changes in the timing of seasonal events (e.g., earlier flowering of plants), and changes in agricultural productivity.Future effects of climate change will vary depending on climate change policies and social development. The two main policies to address climate change are reducing human greenhouse gas emissions (climate change mitigation) and adapting to the impacts of climate change. Geoengineering is another policy option.Near-term climate change policies could significantly affect long-term climate change impacts. Stringent mitigation policies might be able to limit global warming (in 2100) to around 2 °C or below, relative to pre-industrial levels. Without mitigation, increased energy demand and extensive use of fossil fuels might lead to global warming of around 4 °C. Higher magnitudes of global warming would be more difficult to adapt to, and would increase the risk of negative impacts.
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