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the wcrp cmip3 multimodel dataset
the wcrp cmip3 multimodel dataset

... models. For the twenty-first century (computed as the difference of mean temperature for years 2090–99 minus 1980–99), the models show an average warming of 1.8°, 2.8°, and 3.4°C for the low (B1), medium (A1B), and high (A2) forcing scenarios, respectively. For the commitment experiments, by 2100 th ...
Homo Sapiens And The Sixth Mass Extinction Of Species
Homo Sapiens And The Sixth Mass Extinction Of Species

... Forming a thin breathable veneer only slightly more than one thousand the diameter of Earth, and evolving both gradually as well as through major perturbations with time, the Earth’s atmosphere acts as a lungs of the biosphere, allowing an exchange of carbon gases and oxygen with plants and animals, ...
Current Activities and Future Plans for Climate Change
Current Activities and Future Plans for Climate Change

... - Integration of AMDAR into WIGOS - Elaboration of the underpinning/crosscutting role and responsibilities of the instruments and Methods of Observation Programme in the context of WIGOS - Integration of Marine Meteorological and other appropriate Oceanic Observations into the WMO Global Observing S ...
World Bank`s Climate Change Actions in East Asia & Pacific Region
World Bank`s Climate Change Actions in East Asia & Pacific Region

... Rwanda ...
The equilibrium sensitivity of Earth`s temperature to radiation changes.
The equilibrium sensitivity of Earth`s temperature to radiation changes.

... are based on climate change that has been observed over the instrumental period (that is, about the past 150 years). Wigley et al.38 pointed out that uncertainties in forcing and response made it impossible to use observed global temperature changes during that period to constrain S more tightly tha ...
The equilibrium sensitivity of the Earth`s temperature to radiation
The equilibrium sensitivity of the Earth`s temperature to radiation

... are based on climate change that has been observed over the instrumental period (that is, about the past 150 years). Wigley et al.38 pointed out that uncertainties in forcing and response made it impossible to use observed global temperature changes during that period to constrain S more tightly tha ...
Climate Change and Bay Area Microclimates
Climate Change and Bay Area Microclimates

... 69º F in 1930 - 1940, followed by a slow rise to 70º F by 1980 - 1990, and little change thereafter (Figure 9.3C). 4. Average minimum temperature increased irregularly from 45º F for the period from 1910 - 1920, to 47º F in 1960 - 1970, followed by a rise to 48.5º F between 1990 - 2000 (Figure 9.3D ...
Global warming in a nonlinear climate
Global warming in a nonlinear climate

... These deep convective systems have multiple roles in the climate system. They cool the Earth’s surface, leading to significantly lower surface temperatures than would be expected from estimates of pure radiative balance. They transport moisture from the surface to the free atmosphere, and therefore ...
2014年8月16日托福阅读真题回忆
2014年8月16日托福阅读真题回忆

... Paragraph 6: One way to estimate how all the various processes leading to climate variability will combine is by using computer models of the global climate. They can do only so much to represent the full complexity of the global climate and hence may give only limited information about natural vari ...
GE510   properties of complex systems: stability,
GE510 properties of complex systems: stability,

... all ice covered or all melted, then flat) σ = Stefan-Boltzmann constant (W/m2K4) ε = emissivity (unitless – ratio of radiation emitted by a real object to that emitted by an ideal blackbody) ...
Understanding and Applying the Science
Understanding and Applying the Science

... • Can be used to downscale values of temperature and rainfall at a station in terms of values of large scale parameters ...
Four degrees of warming.indd
Four degrees of warming.indd

Advance briefing: IPCC report on climate impacts
Advance briefing: IPCC report on climate impacts

... range of 13°C, but above this it is projected to decrease The health of millions will be impacted, particularly those with low adaptive capacity, through: increases in malnutrition; increased deaths, disease and injury due to heatwaves, floods, storms, fires and droughts; increased diarrhoeal diseas ...
Climate Change-WHO-07
Climate Change-WHO-07

... Earth’s climate is now changing at a pace far outside the range of expected natural variation, and in the opposite direction from what the known, natural, cyclic influences on climate would otherwise be causing at this time. • We should be cooling, but we are warming up: by ~0.8 C in Tavg in the las ...
Slide 1
Slide 1

... Earth’s climate is now changing at a pace far outside the range of expected natural variation, and in the opposite direction from what the known, natural, cyclic influences on climate would otherwise be causing at this time. • We should be cooling, but we are warming up: by ~0.8 C in Tavg in the las ...
UN & GLOBAL WARMING
UN & GLOBAL WARMING

... Programme (UNEP) and the World Meterological Organization (WMO) to assess the scientific knowledge on global warming.  The IPCC concluded in 1990 that there was broad international ...
Meeting the Climate-Change Challenge John P. Holdren
Meeting the Climate-Change Challenge John P. Holdren

... Earth’s climate is now changing at a pace far outside the range of expected natural variation, and in the opposite direction from what the known, natural, cyclic influences on climate would otherwise be causing at this time. • We should be cooling, but we are warming up: by ~0.8 C in Tavg in the las ...
Chapter 3 Powerpoint
Chapter 3 Powerpoint

... 1. CO2 and other gases generated by human activity are responsible for the temperature increase. 2. The average global temperature will continue to rise as emissions of anthropogenic greenhouse gases increase. ...
Interactive comment on “Northern high
Interactive comment on “Northern high

... 2. The authors use a narrow time-window of 6000+/-50 yrs to represent the midHolocene. This is likely to be inappropriate for PMIP data-model comparisons based on simple orbital forcing because at this temporal resolution the reconstruction (but not the model simulation) will also reflect sub-millen ...
Detectability of Streamflow Timing Trends
Detectability of Streamflow Timing Trends

... internal climate variability (the internal oscillations of the climate system). We find that estimated 50year trends in CT due to natural internal climate variability often exceed the trends in CT observed over the last 50 years. Thus, although observed trends in CT may be statistically significant, ...
CGE Hands on training Workshop on Vulnerability and
CGE Hands on training Workshop on Vulnerability and

... country select regions ware made for the years 2010, 2030, 2050, 2100.  For the undergrowth water we take into consideration the increase of the sea level that was obtained with the climate models used.  The deterioration of the undergrowth hydrology reserve only take into consideration the year 2 ...
7.1 - WMO
7.1 - WMO

... which are necessary to incorporate lessons from new measurements and research. ...
present
present

... Urban areas ...
global efforts in addressing climate change
global efforts in addressing climate change

... environmental assessment (SEA) and cumulative effects assessment (CEA) are needed more than ever to incorporate climate issues in policies, programs and plans. To date, we have much yet to do to promote their widespread application by governments and the private sector around the world. Climate data ...
Link - monimet
Link - monimet

... high northern latitudes, between the tundra and temperate forest. The area, which also includes peatlands, plays a significant role in managing global carbon sequestration. In Finland, the EU Life+ MONIMET project aims to better understand climate change by improving access to indicators of regional ...
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Climate sensitivity

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