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Klimaschankungen seit 1700.
Klimaschankungen seit 1700.

... Our discussion of climate variability and climate change at the end of the 19th century leads to a number of conclusions which we consider relevant on methodical, theoretical and practical grounds: (1) The debate on natural climate variability and anthropogenic climate change is not new. A similar d ...
SJ Org. 1 Ann Global Warming in the Arctic x
SJ Org. 1 Ann Global Warming in the Arctic x

...  Global Warming is caused by Greenhouse gases  Scientists now believe Global Warming is caused by humans.  Arctic animals cannot hunt for food because glaciers are melting and there is hardly any snow in the Arctic.  Past the 30 years, the Arctic has warmed twice as much than any place on earth. ...
Climate Change in Africa - Heinrich-Böll
Climate Change in Africa - Heinrich-Böll

... The level of information on the consequences of climate change in Africa has however clearly improved in the last couple of years. The latest IPCC report confirms the continuation of the trend which has become visible on the continent for some time now: rising temperatures as well as, depending on t ...
k7837e
k7837e

... this sector has considerable technical and economic potential for mitigating emissions. In many cases, agricultural mitigation practices also benefit agricultural productivity and resistance, and thus contribute to food security, sustainable development and climate change adaptation. For these reaso ...
Climate Change in Jamaica
Climate Change in Jamaica

Creation Unit 090115
Creation Unit 090115

... differed if they had been living in an LEDC? ...
CLIMATE FORCINGS, FEEDBACKS, AND TELECONNECTIONS IN THE LAND SURFACE-VEGETATION-WATER COMPONENTS OF THE
CLIMATE FORCINGS, FEEDBACKS, AND TELECONNECTIONS IN THE LAND SURFACE-VEGETATION-WATER COMPONENTS OF THE

... warming" with surface heat content" and Davey,C.A., R.A. Pielke Sr., and K.P. Gallo, 2005: Differences between near-surface equivalent temperature and temperature trends for the eastern United States - Equivalent temperature as an alternative measure of heat content." Question: What are the quantita ...
2000 year atmospheric history of methyl chloride from a South Pole
2000 year atmospheric history of methyl chloride from a South Pole

... ice core (solid circles; this study;), Siple Dome, West Antarctica (SDMC) ice core (open circles) [Aydin et al., 2004] The linear regression line through the combined dataset has a slope of 0.027 ppt/yr and an intercept of 442 ppt. Middle-CH3Cl anomaly (DmeanCH3Cl) calculated as a deviation from the ...
Climate Crisis`s Effect on Africa
Climate Crisis`s Effect on Africa

... marginal Sahel region • Small mountain glaciers disappear worldwide potential threat to water supplies in several areas • Coral reef ecosystems extensively and eventually irreversibly damaged ...
pptx - WAIS Divide Ice Core - University of New Hampshire
pptx - WAIS Divide Ice Core - University of New Hampshire

... material (dust, soot from biomass burning, volcanic tephra), (2) soluble material (sea salts, organic compounds, minerals), water (with varying isotopic composition), and atmospheric gases. The layers are compressed into ice when they are buried by more snow. The deeper the ice, the older it is. By ...
MPSAC Climate Change White Paper
MPSAC Climate Change White Paper

Is climate change the number one threat to
Is climate change the number one threat to

... This paper challenges claims that global warming outranks other threats facing humanity  through the foreseeable future (assumed to be 2085–2100). World Health Organization and  British government‐sponsored global impact studies indicate that, relative to other factors,  global warming’s impact on k ...
Climate projections for ecologists
Climate projections for ecologists

... to make informed decisions about their choice of climate model, emissions scenario, baseline period, and data resolution. They will also understand the importance of explicitly stating and justifying their choices, which affect the results and conclusions of their studies. »» For managing biodiversi ...
PDF
PDF

... lifetime of CO2 gas is approximately two years, because that is the average time needed for any CO2 molecule to be incorporated into plants via photosynthesis, mix into ocean or leave the atmosphere by other processes. While the economic downturns in the 1870s and 1930s lasted from 2 to 4 years, thi ...
China’s growth, China’s cities, and the new global low-carbon industrial revolution: November 2010 (347 kB) (opens in new window)
China’s growth, China’s cities, and the new global low-carbon industrial revolution: November 2010 (347 kB) (opens in new window)

... ‘Business as usual’ (BAU) for the next few decades will bring grave risks. Greenhouse gas concentrations (or stocks) have increased to around 435 parts per million (ppm) of carbon-dioxide-equivalent (CO2e). If we continued with BAU for a century we would add at least 300 ppm, taking concentrations t ...
Inaugural Lecture
Inaugural Lecture

... • Atmospheric modelling has long history – first attempts, using computers, made in 1950’s. ...
Environmental problems caused by anthropogenic changes
Environmental problems caused by anthropogenic changes

... Environmental problems caused by anthropogenic changes The principal greenhouse gas is СО2, and the temporal dynamics of its content is relatively well studied. During the industrial epoch there initially occurred slow, and later, the accelerated increase in the content of carbon dioxide in the atm ...
Antarctica and Sea
Antarctica and Sea

... glaciers. The East Antarctic ice sheet appears close to balance, although the ice sheet since the end of the last glacial period (10-20,000 years increased snowfall may cause this area to thicken slowly in future. In ago), or if they are a result of recent climate change caused by human West Antarct ...
Climate Change,Disasters and Security
Climate Change,Disasters and Security

... Main Quest ...
Earth in Yellow Flower
Earth in Yellow Flower

... Tibetan Village: An Obstacle Despite the numerous environmental laws in place and actions taken at the national level to address climate change, very little seems to be occurring at the local level. •This is likely because local governmental officials supposedly fear enforcing environmental laws ...
Folie 1 - Governance of Adaptation
Folie 1 - Governance of Adaptation

... change (adaptive capacity depends on investment potentials)  which means the investment potential determents climate change adaptation strategies and the implementation of measures  Demographic change was regarded as a weak variable (repression, political reasons) Climate change is currently not ...
Presentation: Gender and Climate Change
Presentation: Gender and Climate Change

... Women’s Adaptive Capacity The flood pattern has changed a lot…The laws that used to hold earlier are no more there. We are not able to understand the strange things God is showing us… When summer is supposed to be over and monsoon is supposed to begin, the fields are still burning with heat. But by ...
Challenges and opportunities - Economic Relations Division
Challenges and opportunities - Economic Relations Division

... between adaptation and mitigation. Consequently, the Green climate Fund (GCF) was established in COP-16 in 2010 under the United Nations Framework Convention on Climate Change (UNFCCC). The fund will be available for member countries in coping with and adapting to the effects of climate change. The ...
Climate Change - University of Technology Sydney
Climate Change - University of Technology Sydney

... “We
 offer
 to
 share
 with
 humanity
 our
 Traditional
 Knowledge,
 innovations,
 and
 practices
 relevant
 to
 climate
 change,
 provided
 our
 fundamental
 rights
 as
 intergenerational
 guardians
 of
 this
 knowledge
 are
 fully
recognized
and
respected.
We
reiterate
the
urgent
need
for
collecti ...
Dr. Jorge Cortés-4
Dr. Jorge Cortés-4

... according to different climate models, ranges from 1 to 4°C for the SRES emissions scenario B2 and from 2 to 6°C for scenario A2 (medium confidence). Under future climate change, there is a risk of significant species extinctions in many areas of tropical Latin America (high confidence). The expecte ...
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Global warming



Global warming and climate change are terms for the observed century-scale rise in the average temperature of the Earth's climate system and its related effects.Multiple lines of scientific evidence show that the climate system is warming. Although the increase of near-surface atmospheric temperature is the measure of global warming often reported in the popular press, most of the additional energy stored in the climate system since 1970 has gone into ocean warming. The remainder has melted ice, and warmed the continents and atmosphere. Many of the observed changes since the 1950s are unprecedented over decades to millennia.Scientific understanding of global warming is increasing. The Intergovernmental Panel on Climate Change (IPCC) reported in 2014 that scientists were more than 95% certain that most of global warming is caused by increasing concentrations of greenhouse gases and other human (anthropogenic) activities. Climate model projections summarized in the report indicated that during the 21st century the global surface temperature is likely to rise a further 0.3 to 1.7 °C (0.5 to 3.1 °F) for their lowest emissions scenario using stringent mitigation and 2.6 to 4.8 °C (4.7 to 8.6 °F) for their highest. These findings have been recognized by the national science academies of the major industrialized nations.Future climate change and associated impacts will differ from region to region around the globe. Anticipated effects include warming global temperature, rising sea levels, changing precipitation, and expansion of deserts in the subtropics. Warming is expected to be greatest in the Arctic, with the continuing retreat of glaciers, permafrost and sea ice. Other likely changes include more frequent extreme weather events including heat waves, droughts, heavy rainfall, and heavy snowfall; ocean acidification; and species extinctions due to shifting temperature regimes. Effects significant to humans include the threat to food security from decreasing crop yields and the abandonment of populated areas due to flooding.Possible societal responses to global warming include mitigation by emissions reduction, adaptation to its effects, building systems resilient to its effects, and possible future climate engineering. Most countries are parties to the United Nations Framework Convention on Climate Change (UNFCCC),whose ultimate objective is to prevent dangerous anthropogenic climate change. The UNFCCC have adopted a range of policies designed to reduce greenhouse gas emissions and to assist in adaptation to global warming. Parties to the UNFCCC have agreed that deep cuts in emissions are required, and that future global warming should be limited to below 2.0 °C (3.6 °F) relative to the pre-industrial level.
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