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IM_chapter1 Intro
IM_chapter1 Intro

... Topic 1. Climate Change. One of the major issues facing humanity is climate change. While climate has changed in Earth’s past and has been warmer than even the most dire predictions for how temperatures will increase over the next few centuries, it is human systems that depend on climate being more- ...
Geology-Sheet-3-Carboniferous-Period
Geology-Sheet-3-Carboniferous-Period

... about 12°C today. Later during the Carboniferous, global temperatures cooled to levels similar to today, and there was a great ice age. The composition of the atmosphere was different during the Carboniferous - oxygen (O2) levels were actually much higher 35%, compared with 20% today. Lastly, animal ...
weather quiz - Travelling across time
weather quiz - Travelling across time

... 14. What are scientist who study weather called? Rainologists A. Meteorologists B. Biologists C. 15. Which pressure system brings rain/stormy weather? High pressure A. Low pressure B. 16. __________ is used to photograph and track large scale air movements such as typhoons etc. 17. The process in wh ...
Earth and Space Science Objective Booklet 4a. Compare and
Earth and Space Science Objective Booklet 4a. Compare and

... 4) List five natural products, their sources and their uses. 5) What companies in Mississippi are involved with research and development of new natural products? 4e Explain how the tilt of Earth’s axis and the position of the Earth in relation to the sun determine climatic zones, seasons, and length ...
Diagnosing drought in a changing climate Abigail Swann University
Diagnosing drought in a changing climate Abigail Swann University

... Rising atmospheric CO2 will make Earth warmer, and many studies have inferred that this warming will cause droughts to become more widespread and severe. However, rising atmospheric CO2 also modifies stomatal conductance and plant water use, processes that are often are overlooked in impact analysis ...
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O 3

... • Exosphere: The outer limits of earth’s atmosphere. – The interface between earth and space. ...
Class #1: Introduction, Energy
Class #1: Introduction, Energy

... Overview of the Earth’s Atmosphere • The Early Atmosphere – The Earth’s first atmosphere was composed mostly of hydrogen and helium. – The atmosphere evolved due to outgassing of CO2 and H2O from the cooling center of the Earth causing rain and eventually lakes and oceans. – Lakes and oceans acted ...
landscapes
landscapes

... having a characteristic shape, and produced by natural causes; it includes major forms such as a plain, plateau, or mountain, and minor forms such as a hill, valley, slope, esker, or dune. Taken together, the landforms make up the surface configuration of the earth." - Glossary of Geology ...
integrating observed, inferred and simulated data to
integrating observed, inferred and simulated data to

... reconstruct and examine the eutrophication history of a lake in southwest Ireland over a c.60-year period and uses computer models to simulate future responses in water quality as a result of projected changes in land use and climate. The study site, Lough Leane, has major national and international ...
1-2 Notes: Continental Drift Continents Join Together and Split Apart
1-2 Notes: Continental Drift Continents Join Together and Split Apart

...  The types of rock found in Brazil perfectly match rock found in western Africa.  Limestone layers in the eastern U.S. match limestone layers found in Scotland. Pangaea and Continental Drift  The continents were once joined in a huge supercontinent called Pangaea.  The word Pangaea comes from th ...
Nature`s Fury Educator`s Guide - American Museum of Natural History
Nature`s Fury Educator`s Guide - American Museum of Natural History

... Earthquakes: Scientists use a global network of seismometers to measure seismic activity. To calculate the probability that an earthquake will occur, they consult records of past events and use the Global Positioning System (GPS) to track plate movements. ...
MS-ESS2-1 Earth`s Systems - Next Generation Science Standards
MS-ESS2-1 Earth`s Systems - Next Generation Science Standards

... from regions of high pressure to low pressure, causing weather (defined by temperature, pressure, humidity, precipitation, and wind) at a fixed location to change over time, and how sudden changes in weather can result when different air masses collide. Emphasis is on how weather can be predicted wi ...
thesis paper - The Ohio State University
thesis paper - The Ohio State University

... wedge. The release of water, in particular, from the subducting plate triggers melting as it rises upwards through the mantle wedge. Once the mantle begins to melt, the molten material rises to the surface creating a volcano above the subduction zone. Figure 1 provides a visual summary of the magma ...
They believe that 200 million years ago, some force made Pangaea
They believe that 200 million years ago, some force made Pangaea

...  The rest is fresh water, or water without salt. Most of that is frozen at the poles.  Fresh water comes from lakes, rivers, and rain. Much fresh water, called groundwater, is stored in the soil.  People need fresh water—the Earth has enough, but some places have too much, and others have too lit ...
australia`s world heritage places - willandra lakes information sheet
australia`s world heritage places - willandra lakes information sheet

... Thousands of years ago it was a beautiful paradise filled with water, animals, birds and human activity. This region has revealed ancient human bones, footprints and animal fossils that help scientists understand what life was like many years ago ...
FREE Sample Here
FREE Sample Here

... nitrous oxide (N2O). water vapor (H2O). methane (CH4). chlorofluorocarbons (CFCs). ...
Section 2 - Burnet Middle School
Section 2 - Burnet Middle School

... • Mountain peaks are cold and have snow even in the Tropics because high mountain air is thin and cannot hold heat. • Mountains have an effect—called a rain shadow—whereby they block rain from reaching interior regions. ...
FREE Sample Here
FREE Sample Here

... nitrous oxide (N2O). water vapor (H2O). methane (CH4). chlorofluorocarbons (CFCs). ...
Meteorology Today 10E
Meteorology Today 10E

... Much of Tibet lies at altitudes over 18,000 feet where the pressure is about 500 mb. At such altitudes, the Tibetans are above roughly a. 10 percent of the air molecules in the atmosphere. b. 25 percent of the air molecules in the atmosphere. c. 50 percent of the air molecules in the atmosphere. d. ...
the MSWord file, in  format.
the MSWord file, in format.

... Thought questions: what is the difference between weather and climate? From my all time favorite blog – www.wasatchweatherweenies by Jim Steenburgh of UofU meteorology… from what meteorologists quip: “Climate is what you expect… weather is what you get.” Content Some Terms:  CLIMATE... long-term we ...
Earth and Atmosphere
Earth and Atmosphere

... • This is rather like the atmosphere on Mars and Venus today. • The Earth’s atmosphere would also have contained water vapour which condensed to form the oceans. ...
Earth Science
Earth Science

... addition of heat and pressure causing a partial melting of some of the minerals in the sediment. This process is referred to as metamorphism and results in creation of a metamorphic rock. The straight arrows within the rock cycle diagram indicate that any one rock type can turn into any other rock t ...
Brilliant “Morning Star” and “Evening Star”
Brilliant “Morning Star” and “Evening Star”

... relatively more water vapor • The greenhouse effect of the water vapor raised the temperature, and more liquid water evaporated • This further intensified the greenhouse effect, and raised the temperature even higher • This runaway process continued until oceans disappeared • Almost all of the water ...
Academic Earth/Space Science Date: March 19, 2014 ET Topic: U
Academic Earth/Space Science Date: March 19, 2014 ET Topic: U

... Analyze physical patterns of motion to make predictions or draw conclusions (e.g., solar system, tectonic plates, weather systems, atomic motion, waves). S11.D.2.1.1 -- Important Describe how changes in concentration of minor components (e.g., O2, CO2, ozone, dust, pollution) in Earth's atmosphere a ...
Glaciers - Firelands Local Schools
Glaciers - Firelands Local Schools

... 1. Glaciers flow unevenly beneath the surface, causing regions of tension & compression under brittle surface a. This results in large cracks, crevasses, that form on the surface 2. Some parts of the ice sheets may move out over the ocean & form ice shelves. a. When tides rise and fall, large blocks ...
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History of climate change science



The history of the scientific discovery of climate change began in the early 19th century when ice ages and other natural changes in paleoclimate were first suspected and the natural greenhouse effect first identified. In the late 19th century, scientists first argued that human emissions of greenhouse gases could change the climate. Many other theories of climate change were advanced, involving forces from volcanism to solar variation. In the 1960s, the warming effect of carbon dioxide gas became increasingly convincing, although some scientists also pointed out that human activities, in the form of atmospheric aerosols (e.g., ""pollution""), could have cooling effects as well. During the 1970s, scientific opinion increasingly favored the warming viewpoint. By the 1990s, as a result of improving fidelity of computer models and observational work confirming the Milankovitch theory of the ice ages, a consensus position formed: greenhouse gases were deeply involved in most climate changes, and human emissions were bringing serious global warming.Since the 1990s, scientific research on climate change has included multiple disciplines and has expanded, significantly increasing our understanding of causal relations, links with historic data and ability to numerically model climate change. The most recent work has been summarized in the Assessment Reports by the Intergovernmental Panel on Climate Change. Climate change is a significant and lasting change in the statistical distribution of weather patterns over periods ranging from decades to millions of years. It may be a change in average weather conditions, or in the distribution of weather around the average conditions (i.e., more or fewer extreme weather events). Climate change is caused by factors that include oceanic processes (such as oceanic circulation), biotic processes, variations in solar radiation received by Earth, plate tectonics and volcanic eruptions, and human-induced alterations of the natural world; these latter effects are currently causing global warming, and ""climate change"" is often used to describe human-specific impacts.
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