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south afriCa`s ChanGinG Climate - Allergy Society of South Africa
south afriCa`s ChanGinG Climate - Allergy Society of South Africa

... This initial modelling showed that, within the next hundred years, ‘... the bioclimate of the country shows warming and aridification trends which are sufficient to shrink the area amenable to the country’s biomes to between 38% and 55% of their current combined (regional) coverage. The largest loss ...
Rapid and significant sea-level rise expected if global warming
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... rise is a delayed and complex response to past temperatures, sea levels will continue to climb for centuries into the future, even after concentrations of greenhouse gases in the atmosphere have been stabilised. This study, partly conducted under the EU RISES-AM project1, projected sea-level rise ar ...
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... This comment addresses the CCSP’s unproven attribution of climate change to manmade influences, specifically from key finding #1: “1. Human-induced climate change and its impacts are apparent now throughout the United States. • Global warming is unequivocal and is due primarily to human-induced emis ...
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... large fluctuations are common to the climate system. A thousand years ago temperatures were apparently higher than today and it was during this period that the Vikings colonized Greenland. We note that the temperatures in the eighteenth and nineteenth centuries were unusually cool, for which we have ...
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...  Anthropogenic emissions are kept constant at 2006 levels  Sensitivity simulation which zeros out Asian anthropogenic emissions to separate Asian ozone (only 3 years) * Linkage between CAM and GEOS-Chem was originally developed by Kim et al. (2015), and updated to v9-02 by Evan Couzo. ...
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7.6 mb full presentation with graphics

... Climate change stronger and sooner • Global carbon dioxide emissions from fossil fuel have accelerated since 2000 • Rise in 1990s: 0.7%/yr; 2.9% since 2000 • Three causes: growth in world economy, rise of coal use in China, weakening of natural carbon sinks (forests, seas, soils) • Growth in atmosph ...
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... In  preparation  for  COP21,  Professors  of  Law  Alain  Supiot  and  Mireille  Delmas-­‐‑Martyi  of  the   Collége  de  France,    and  Pierre  Calame,  former  Director  of  the  Foundation  for  the  Progress  of   Humankind,  Paris,  1  collaborated    for  the  development  of  law  for  clima ...
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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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