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Chapter 3 Review Questions Knowledge 1. The Big Rock at Okotoks
Chapter 3 Review Questions Knowledge 1. The Big Rock at Okotoks

... concentration and the average temperature. Average temperature is determined by analyzing oxygen-18: oxygen-16 ratios, while concentrations of carbon dioxide can be measured from little bubbles of atmospheric gases trapped in annual ice layers. People are mainly adding to the atmospheric carbon diox ...
Global Warming May Cause Sea Levels to Rise 34 Centimeters by
Global Warming May Cause Sea Levels to Rise 34 Centimeters by

... the end of the century, causing increased flooding and coastal erosion, according to a new study by Australian researchers. The study -- published in this month's issue of the journal Geophysical Research Letters -- said global warming was expected to further heat up the world's oceans and cause gla ...
Global Climate Change - Worth County Schools
Global Climate Change - Worth County Schools

...  Human activities – any activity that releases “greenhouse gases” into the atmosphere ...
What are the risks of a changing climate?
What are the risks of a changing climate?

... with the rim of the glass. 2. Fill another glass (#2) with ice so it is higher than the edge of glass. 3. Fill glass #2 with water. 4. As ice melts, what is the difference between the levels of glass #1 versus glass #2? ...
National Geographic - u.arizona.edu
National Geographic - u.arizona.edu

... There are no words, though, to describe how much, and how fast, the ice is changing. Researchers long ago predicted that the most visible impacts from a globally warmer world would occur first at high latitudes: rising air and sea temperatures, earlier snowmelt, later ice freeze-up, reductions in s ...
global climate change
global climate change

... present time, the tilt of the Earth's axis is 23.5°. When the tilt is small there is less climatic variation between the summer and winter seasons in the middle and high latitudes. Winters tend to be milder and summers cooler. ...
Global Environmental Change
Global Environmental Change

... Climate change is intensifying the circulation of water on, above and below the surface of the Earth — causing drought and floods to be more frequent, severe and widespread. Higher temperatures increase the amount of moisture that evaporates from land and water, leading to drought in many areas. Lan ...
Midterm 3 Review
Midterm 3 Review

... • Rapid increase of greenhouse gases (CO2, CH4, N2O) since 1750: far exceed pre-industrial values determined from ice core measurements spanning the last 650,000 years, which is mainly caused by CO2 fossil fuel use. Lead to strong radiative heating. • The developed countries and developing countries ...
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 - Cloudfront.net
Climate Change - Cloudfront.net

... warming 2. Short term warming and long term cooling 3. No effects to the atmosphere ...
Planning meeting
Planning meeting

... Antarctic marine ecosystem…We now recognize the west Antarctic Peninsula (WAP) as a premier example of a climatesensitive region experiencing major changes in species abundance and composition due to changes in range and distribution that are occurring in response to regional climate change manifest ...
Timmermann's PowerPoint
Timmermann's PowerPoint

... The observed recent warming hiatus, defined as the reduction in GMST trend during 1998–2012 as compared to the trend during 1951– 2012, is attributable in roughly equal measure to a cooling contribution from internal variability and a reduced trend in external forcing (expert judgment, medium confid ...
2Dclimate / Uploaded File
2Dclimate / Uploaded File

... – Anywhere pollen can be found, it will tell you the plant species that lived around the location at the time the sediments were deposited, thus the temperature range at the time of deposition ...
11.2 Human Activity and Climate Change (change in long term
11.2 Human Activity and Climate Change (change in long term

...  What has a higher albedo: sea ice or soil? ...
Proxy Climate Data - The Department of Geological Sciences
Proxy Climate Data - The Department of Geological Sciences

... 1. Chief instigator of climate change was earth orbital change, a very weak forcing. 2. Chief mechanisms of Pleistocene climate change are GHGs & ice sheet area, as feedbacks. 3. Climate on long time scales is very sensitive to even small forcings. 4. Human-made forcings dwarf natural forcings that ...
Prehistoric Era Overview
Prehistoric Era Overview

... action exposed land that had been under water. Sea levels rose in periods of warming, creating islands where dry land had been. The picture of climate change over the past 70,000 years is a general trend of cooler temperatures than today. Since about 20,000 years ago, however, the climate has been w ...
Topic 8.6 Global Warming
Topic 8.6 Global Warming

... Republic of China, Japan and South Korea in 2005. It is an agreement in which the signatory nations agree to cooperate in reducing emissions. It has been criticized as worthless because the reductions are voluntary. It has been defended because it includes China and India, major greenhouse gas produ ...
Find some land, build a house?
Find some land, build a house?

... formed 11,000 years ago at the end of the last ice age. ...
FAQ 6.1 | Could Rapid Release of Methane and Carbon
FAQ 6.1 | Could Rapid Release of Methane and Carbon

... relicts from the last glaciation, and hold at least twice the amount of carbon currently present in the atmosphere as carbon dioxide (CO2). Should a sizeable fraction of this carbon be released as methane and CO2, it would increase atmospheric concentrations, which would lead to higher atmospheric t ...
Summary report by the Chair
Summary report by the Chair

... glaciers; the decreasing trends in Arctic sea ice and northern hemisphere spring snow cover; and the likelihood of these impacts intensifying as global mean surface temperature rises. On permafrost, he mentioned that there is high confidence that permafrost temperature have increased in most regions ...
Category 1: Increasingly Severe Weather
Category 1: Increasingly Severe Weather

... where they have lived is an unchanging thing, and has always remained a constant. Climate terms might include hot, temperate, mild, harsh, freezing, wet, humid, cold, or for those lucky enough to live in San Diego- “perfect”. Discussions about climate would likely include the use of the word “averag ...
file
file

... themselves. As humans continue to exterminate the ancient trees, plants and animals of these magnificent and precious rain forests leaving only dust bowls in their wake, tremendous amounts of carbon is released into the atmosphere instead of water vapour. The consequences are catastrophic changes in ...
Anthropogenic Contributions to Future Sea Level and
Anthropogenic Contributions to Future Sea Level and

... were contributing to the rising sea level most, but glaciers. For three different initial volumes of glacial ice, glacial outpaced ice cap water for the next 600 years. ...
Global Warming and Climate Change in a Nutshell
Global Warming and Climate Change in a Nutshell

... the Greenland, Arctic and Antarctic ice melting may be happening at a nonlinear rate, not at the linear rate used by the IPCC. They believe that the melting is occurring 10 times faster than the IPCC estimated. This higher rate of melt may block the oceans’ “overturning circulation,” which in turn, ...
Sea-Ice Melting & Coastal Erosion
Sea-Ice Melting & Coastal Erosion

... increasing wave-induced erosion along Arctic shores. When the buffer provided by the shore ice has been lost, the full force of ocean waves are allowed to surge against the coastline and coastal villages. ...
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Climate change in the Arctic

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