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The Earth`s atmosphere and climate.
The Earth`s atmosphere and climate.

... Why was the Cretaceous so warm? A period of Greenhouse Earth. Rapid rates of seafloor spreading suggest high rates of magma delivery to the Earth’s surface via volcanoes; including large volumes of CO2 that accumulated in the atmosphere. Elevated CO2 concentrations caused a positive radiative forci ...
Special Rapporteur on adequate housing as a component of
Special Rapporteur on adequate housing as a component of

... I thank you for the opportunity to be here and to share with you my views on the impact of climate change on the fulfillment of the right to adequate housing. During the presentation of my previous report to the General Assembly last year, I expressed my great interest on this subject. It is now evi ...
Climate Change overview File
Climate Change overview File

... Radiation that has a wavelength that is longer than that of visible light, but shorter than that of radio waves ...
chapter 20 power point
chapter 20 power point

... Radiation that has a wavelength that is longer than that of visible light, but shorter than that of radio waves ...
EEA HU04 Adaptation Programme ADAPTATION to CLIMATE
EEA HU04 Adaptation Programme ADAPTATION to CLIMATE

... •Excess mortality caused by extreme heath waves •Road accidents •tourism ...
it`s not the heat, it`s the tepidity
it`s not the heat, it`s the tepidity

... growing food or working outdoors in some areas for parts of the year. The precise levels of climate change sufficient to trigger tipping points remain uncertain, but the risk associated with crossing multiple tipping points in the earth system or in interlinked human and natural systems increases wi ...
Sea Level Changes and the Texas Coastal Environment
Sea Level Changes and the Texas Coastal Environment

... dioxide emissions. Transportation is responsible for 32 percent of carbon dioxide emissions. Before the Industrial Revolution, CO2 levels in the atmosphere were 280 ppm (parts per million). By 1958, the level was 315 ppm and today’s levels are nearly 380 ppm (Fig. 3). Scientific reports from 2007 sh ...
ch20 - Napa Valley College
ch20 - Napa Valley College

... Radiation that has a wavelength that is longer than that of visible light, but shorter than that of radio waves ...
Download case study as PDF
Download case study as PDF

... environmental systems — are already vulnerable to the stresses that result from military occupation and conflict. These stresses include poverty and harmful occupational practices such as land appropriation and restrictions on access and movement. ...
2. arctic warming and its consequences have major implications for
2. arctic warming and its consequences have major implications for

... A second pathway by which Arctic processes can amplify changes in global climate is through alterations in ocean circulation patterns. One of the ways the Sun's energy is transported from the equator toward the poles is through the globally interconnected movement of ocean waters known as the thermo ...
Temperature Variation
Temperature Variation

... a. Warms the troposphere, water vapor and CO2 absorb infrared heat radiated by Earth’s surface b. Greenhouse effect + natural cooling of evaporation and condensation allow Earth to be habitable c. Other gases: Methane, Nitrous Oxide; CFC’s 18-2 Climate Change and Human Activities -What is Global War ...
Global Change Impact Studies Centre and its Activities
Global Change Impact Studies Centre and its Activities

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Detection

... sulphate aerosols, and (c) with all forcings, both natural and anthropogenic. The thick line shows the instrumental data while the thin lines show the individual model simulations in the ensemble of four members. Note that the data are annual mean values. The model data are only sampled at the locat ...
non-co2 greenhouse gas emissions from oil refineries
non-co2 greenhouse gas emissions from oil refineries

... No part of this book may be reproduced by any means, or transmitted or translated into a machine language without the written permission of the publisher. The information contained in this publication is provided as guidance only and while every reasonable care has been taken to ensure the accuracy ...
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PDF

... temperature, these effects are generally unfavorable at low (tropical) latitudes and favorable at high latitudes. The most important beneficial effects are on the growth of wheat in Canada, Northern Europe and Russia (Smit, Ludlow and Brklacich 1988; Parry, Rosenzweig, and Livermore 2005). The aggr ...
IPRC News
IPRC News

... has the frequency of weather conditions, such as Kona Lows, that produce heavy rainfall events over Hawai‘i. These are the conclusions of IPRC’s Assistant Researcher Oliver Elison Timm, who has been studying the effects of climate change on rainfall, drought, and evapotranspiration across the Hawaii ...
Europeans` perceptions of climate change and global warming: A
Europeans` perceptions of climate change and global warming: A

... The European countries and also the European Union have been a driving force in the field of climate policy. A couple of really ambitious decisions have been made, for instance a reduction of CO-2 emission of 20% by 2020 and even of 30% if an international agreement can be achieved. These announceme ...
Key Elements for Success on Climate Change Mitigation at COP21
Key Elements for Success on Climate Change Mitigation at COP21

... Former Director, UN DESA’s Population Division, USA. ...
The trouble with negative emissions
The trouble with negative emissions

UNEP Adaptation Source book (2008)
UNEP Adaptation Source book (2008)

... Boko, M., I. Niang, A. Nyong, C. Vogel, A. Githeko, M. Medany, B. Osman-Elasha, R. Tabo and P. Yanda, 2007: Africa. Climate Change 2007: Impacts, Adaptation and vulnerability. Contribution of Working Group II to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, M.L. Parr ...
CLIMATE CHANGE: IMPLICATIONS FOR COMMERCIAL
CLIMATE CHANGE: IMPLICATIONS FOR COMMERCIAL

... Adaptation, Not Mitigation, Is Increasingly Accepted26 as The Proper Focus When Dealing With Negative Impacts Of Climate Change A. ...
CLIMATE CHANGE A Natural Hazard
CLIMATE CHANGE A Natural Hazard

... World Climate Conference held in Geneva in 1990 and the accompanying Ministerial Declaration called for UN action to negotiate a convention that would establish international agreements necessary to avoid dangerous climate change. The UN Framework Convention on Climate Change (UNFCCC) and its Kyoto ...
UNDP-GEF Adaptation
UNDP-GEF Adaptation

... Conference of the Parties (COP) • highest decision-making authority of the UNFCCC Subsidiary Body for Scientific & Technological Advice (SBSTA) • provides link between scientific information and policy needs of COP Subsidiary Body for Implementation (SBI) • advises on implementation issues Global En ...
The UN Climate Change Conference, 2009 (COP 15) ACCA POsiTiON PAPer
The UN Climate Change Conference, 2009 (COP 15) ACCA POsiTiON PAPer

... countries alone will not be enough to tackle climate change, as emerging economies such as Brazil, China and India become increasingly significant emitters of greenhouse gases. Although emissions per person are much lower in developing than developed countries, they are likely to grow exponentially ...
'An Economist Tries to Grapple with Catastrophic Climate Change' (pdf).
'An Economist Tries to Grapple with Catastrophic Climate Change' (pdf).

... after the fact, we concoct an explanation that makes it appear less random, and more predictable than it was – Nassim Taleb _________________________________________ The climate system is an angry beast and we are poking it with sticks – Wally Broecker ...
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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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