Climate Change and Forest Fire Potential in Russian and Canadian
... Climate warming of the magnitude projected can be expected to have major impacts on the forests of northern circumpolar countries. Based on GCM projections largescale shifting of forest vegetation northward is expected (Solomon and Leemans, 1989; Rizzo and Wilken, 1992; Smith and Shugart, 1993), at ...
... Climate warming of the magnitude projected can be expected to have major impacts on the forests of northern circumpolar countries. Based on GCM projections largescale shifting of forest vegetation northward is expected (Solomon and Leemans, 1989; Rizzo and Wilken, 1992; Smith and Shugart, 1993), at ...
IPCC launches complete Synthesis Report
... endorses these reports in a dialogue between the governments that request the reports and will work with them and the scientists that write them. In this discussion the scientists have the last word on any additions or changes, although the Panel may agree by consensus to delete something. The Fifth ...
... endorses these reports in a dialogue between the governments that request the reports and will work with them and the scientists that write them. In this discussion the scientists have the last word on any additions or changes, although the Panel may agree by consensus to delete something. The Fifth ...
Climate change and wildlife diseases: When does the host matter
... Lips et al. (2008); specifically, a reanalysis of mortality data suggested that multiple introductions of B. dendrobatidis, coupled with its spatial spread along mountain ranges, better explained the timing of harlequin frog die-offs (Lips et al. 2008). It is important to note that warmer temperature ...
... Lips et al. (2008); specifically, a reanalysis of mortality data suggested that multiple introductions of B. dendrobatidis, coupled with its spatial spread along mountain ranges, better explained the timing of harlequin frog die-offs (Lips et al. 2008). It is important to note that warmer temperature ...
Comment by: Patrick J. Michaels and Paul C. Knappenberger
... determination reflected a greater degree of certainty that a low ECS value could be excluded than did the IPCC. From the IWG2010 (p. 14): “Finally, we note the IPCC judgment that the equilibrium climate sensitivity “is very likely larger than 1.5°C.” Although the calibrated Roe & Baker distribution, ...
... determination reflected a greater degree of certainty that a low ECS value could be excluded than did the IPCC. From the IWG2010 (p. 14): “Finally, we note the IPCC judgment that the equilibrium climate sensitivity “is very likely larger than 1.5°C.” Although the calibrated Roe & Baker distribution, ...
160309_BIS_slides_final_for_websites (opens in new window)
... The transition to the low-carbon economy in the context of urban development and technological change presents huge investment opportunities: infrastructure alone requires $4-6 trillion p.a. over next two decades. Should try to make all investment sustainable/green from now on: sustainable/green sho ...
... The transition to the low-carbon economy in the context of urban development and technological change presents huge investment opportunities: infrastructure alone requires $4-6 trillion p.a. over next two decades. Should try to make all investment sustainable/green from now on: sustainable/green sho ...
Junk to Green Funk
... Regardless of the debate what do we know is happening for sure? Using the paragraphs below, discuss what is already changing. Using a large map, look at which countries appear to be suffering the most. Are they the rich or the poor countries? “Beyond the Heart of the World, the Younger Brother is ch ...
... Regardless of the debate what do we know is happening for sure? Using the paragraphs below, discuss what is already changing. Using a large map, look at which countries appear to be suffering the most. Are they the rich or the poor countries? “Beyond the Heart of the World, the Younger Brother is ch ...
Fertilization and Carbon Sequestration in BC Forests
... The BC MFR currently projects a 15 cubic metre (m ) per hectare (ha) response to fertilization by Interior spruce and Douglas-fir, and a 30 m3/ha response by coastal Douglas-fir. The relationships of 1 m3 of wood containing 0.25 tonnes of C and 1 tonne of stored carbon removing 3.67 tonnes of CO2 fr ...
... The BC MFR currently projects a 15 cubic metre (m ) per hectare (ha) response to fertilization by Interior spruce and Douglas-fir, and a 30 m3/ha response by coastal Douglas-fir. The relationships of 1 m3 of wood containing 0.25 tonnes of C and 1 tonne of stored carbon removing 3.67 tonnes of CO2 fr ...
Annex III
... The radiative forcing from such interactions has traditionally been attributed to numerous indirect aerosol effects, but in this report, only two levels of radiative forcing (or effect) are distinguished: Radiative forcing (or effect) due to aerosol-cloud interactions (RFaci) The radiative forcing ( ...
... The radiative forcing from such interactions has traditionally been attributed to numerous indirect aerosol effects, but in this report, only two levels of radiative forcing (or effect) are distinguished: Radiative forcing (or effect) due to aerosol-cloud interactions (RFaci) The radiative forcing ( ...
3 - Environmental Intermediate
... The atmosphere is the name for a layer of gases that surround a body of sufficiently large mass. The gases are attracted by the gravity of the body, and held fast if gravity is sufficient (thaerefore mass must be large) and the atmosphere's temperature is low. Some planets (called gas giants) consis ...
... The atmosphere is the name for a layer of gases that surround a body of sufficiently large mass. The gases are attracted by the gravity of the body, and held fast if gravity is sufficient (thaerefore mass must be large) and the atmosphere's temperature is low. Some planets (called gas giants) consis ...
Climate Change in Mongolia
... Japan. This dataset is composed of two types of model output: global climate model outputs and regional climate model outputs. The global climate model outputs (hereinafter referred to as “GCM data” ) are the results of calculations using an atmospheric model covering the entire world with an image ...
... Japan. This dataset is composed of two types of model output: global climate model outputs and regional climate model outputs. The global climate model outputs (hereinafter referred to as “GCM data” ) are the results of calculations using an atmospheric model covering the entire world with an image ...
Annual Progress Report 2015-16
... over the western and central Indian regions are not specified. In the present study, the simulations of WRF-CHEM for different schemes are compared with the observations to investigate the suitable schemes over the western and central Indian region. The model simulations were performed for the year ...
... over the western and central Indian regions are not specified. In the present study, the simulations of WRF-CHEM for different schemes are compared with the observations to investigate the suitable schemes over the western and central Indian region. The model simulations were performed for the year ...
Impacts of Climate Change on Tourism in the Mediterranean
... mass travelers of the 1960;s and 70;s, and are today ‘s discerning and sophisticated travelers with the means and the will to travel. Increasingly they are looking at long-haul destinations, one of the fastest segments of the travel trade, since they are already familiar with many European resorts ...
... mass travelers of the 1960;s and 70;s, and are today ‘s discerning and sophisticated travelers with the means and the will to travel. Increasingly they are looking at long-haul destinations, one of the fastest segments of the travel trade, since they are already familiar with many European resorts ...
Impacts of Climate Change on Water Resources in Idaho
... Impacts of Climate Change on Water Resources in Idaho ...
... Impacts of Climate Change on Water Resources in Idaho ...
Planning for climate change adaptation: North Doddington Farm
... Planting 800 m of new shelter belt (shown in green on the farm map). Primarily intended to act as a windbreak, this will reduce the risk of soil erosion. It will also provide some shelter for livestock, which will reduce the risk of heat stress in hotter spells. Further actions are being considere ...
... Planting 800 m of new shelter belt (shown in green on the farm map). Primarily intended to act as a windbreak, this will reduce the risk of soil erosion. It will also provide some shelter for livestock, which will reduce the risk of heat stress in hotter spells. Further actions are being considere ...
Major in Atmosphere and Climate
... tornadoes and hurricanes to investigating and understanding them to become an expert. You would like to gain a quantitative understanding of climate processes and their interactions – ranging from the molecular to the global scale and from short-lived phenomena to changes over millions of years, and ...
... tornadoes and hurricanes to investigating and understanding them to become an expert. You would like to gain a quantitative understanding of climate processes and their interactions – ranging from the molecular to the global scale and from short-lived phenomena to changes over millions of years, and ...
The role of biospheric feedbacks in the simulation of the... historical land cover change on the Australian January climate
... Received 27 July 2003; revised 16 September 2003; accepted 25 September 2003; published 26 November 2003. ...
... Received 27 July 2003; revised 16 September 2003; accepted 25 September 2003; published 26 November 2003. ...
Stephen Schneider 1945–2010 A Biographical Memoir by B. D. Santer
... thought experiments that could not be conducted in the real world. How might Earth’s climate respond to human-caused changes in atmospheric levels of greenhouse gases? Could models provide credible estimates of the climate of the Cretaceous? How does the climate system respond to massive volcanic er ...
... thought experiments that could not be conducted in the real world. How might Earth’s climate respond to human-caused changes in atmospheric levels of greenhouse gases? Could models provide credible estimates of the climate of the Cretaceous? How does the climate system respond to massive volcanic er ...
Climate Change & Sustainable Development in Africa
... • Crop revenues will likely fall by as much as 90% by 2100 with small scale farmers being the most affected • In Egypt, for example, climate change could decrease national production of many crops (ranging from -11% for rice to -28% for soybeans) by the year 2050 ...
... • Crop revenues will likely fall by as much as 90% by 2100 with small scale farmers being the most affected • In Egypt, for example, climate change could decrease national production of many crops (ranging from -11% for rice to -28% for soybeans) by the year 2050 ...
What`s New in TerrSet
... generate a projected land cover map for a future date (lower-center). In addition, LCM can generate a soft projection—a map of the vulnerability to land transition (upper-right). ...
... generate a projected land cover map for a future date (lower-center). In addition, LCM can generate a soft projection—a map of the vulnerability to land transition (upper-right). ...
Consequences of Global Warming of 1.5 °C and 2 °C for Regional
... highlighting its feasibility and impacts are beginning to emerge [10–13]. Under most low emission scenarios, global warming overshoots 1.5˚C some time during the 21st century before dropping to this limit around or after 2100 [11]. As a result, 1.5˚C is considered an aspirational ‘long-term’ tempera ...
... highlighting its feasibility and impacts are beginning to emerge [10–13]. Under most low emission scenarios, global warming overshoots 1.5˚C some time during the 21st century before dropping to this limit around or after 2100 [11]. As a result, 1.5˚C is considered an aspirational ‘long-term’ tempera ...
Climate change feedback
Climate change feedback is important in the understanding of global warming because feedback processes may amplify or diminish the effect of each climate forcing, and so play an important part in determining the climate sensitivity and future climate state. Feedback in general is the process in which changing one quantity changes a second quantity, and the change in the second quantity in turn changes the first. Positive feedback amplifies the change in the first quantity while negative feedback reduces it.The term ""forcing"" means a change which may ""push"" the climate system in the direction of warming or cooling. An example of a climate forcing is increased atmospheric concentrations of greenhouse gases. By definition, forcings are external to the climate system while feedbacks are internal; in essence, feedbacks represent the internal processes of the system. Some feedbacks may act in relative isolation to the rest of the climate system; others may be tightly coupled; hence it may be difficult to tell just how much a particular process contributes. Forcings, feedbacks and the dynamics of the climate system determine how much and how fast the climate changes. The main positive feedback in global warming is the tendency of warming to increase the amount of water vapor in the atmosphere, which in turn leads to further warming. The main negative feedback comes from the Stefan–Boltzmann law, the amount of heat radiated from the Earth into space changes with the fourth power of the temperature of Earth's surface and atmosphere.Some observed and potential effects of global warming are positive feedbacks, which contribute directly to further global warming. The Intergovernmental Panel on Climate Change's (IPCC) Fourth Assessment Report states that ""Anthropogenic warming could lead to some effects that are abrupt or irreversible, depending upon the rate and magnitude of the climate change.""