AmplifyScience Earth’s Changing Climate Sample Lessons ...
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Investigation NotebookEarth’s Changing Climate Sample Lessons
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Earth’s Changing Climate—Lesson 1
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Table of Contents
Lesson 1: Introduction to Climate Change . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3
Warm-Up: Anticipation Guide . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3
Analyzing Climate Data . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4
Evidence Gradient . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 5
Homework: Reading The Effects of Climate Change Article Set . . . . . . 6
Article Set: The Effects of Climate Change . . . . . . . . . . . . . . . . . . . . . . . . . 7
Lesson 2: Exploring Energy in the Earth System . . . . . . . . . . . . . . . . . . . . . . . . . . 15
Warm-Up . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 15
Exploring Earth’s Changing Climate Simulation . . . . . . . . . . . . . . . . . . . 16
Making a Claim About Melting Ice . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 18
Lesson 3: Testing Changes to the Atmosphere . . . . . . . . . . . . . . . . . . . . . . . . . . . 20
Warm-Up . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 20
Testing Nitrogen Dioxide and Carbon Dioxide in the Sim . . . . . . . . . . . 21
Testing Sulfur Dioxide and Methane in the Sim . . . . . . . . . . . . . . . . . . . 22
Analyzing Evidence from the Sim Tests . . . . . . . . . . . . . . . . . . . . . . . . . . 23
Answering the Investigation Question . . . . . . . . . . . . . . . . . . . . . . . . . . . 25
Article: “A Hole in Earth’s Ozone Layer” . . . . . . . . . . . . . . . . . . . . . . . . . . 27
Earth’s Changing Climate Glossary . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 29
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Lesson 1: Introduction to Climate Change Warm-Up: Anticipation Guide
For each statement below, circle whether you agree or disagree . Be prepared to
share your explanations with a partner .
Don’t worry about whether your answers are right or wrong . This is an opportunity to
think about what you already know about Earth’s changing climate .
1 . Earth’s atmosphere is made of different gases that can affect Earth’s climate in different ways .
agree disagree
2 . Climate has to do with how much energy is in the Earth system . agree disagree
3 . Earth’s atmosphere does not changeagree disagree
4 . There have been times in the past when Earth’s climate was very different .
agree disagree
5 . Energy from the sun that enters the Earth system does not leave . agree disagree
6 . It is possible for gases in the atmosphere to change the behavior of energy on Earth .
agree disagree
7 . Human actions cannot change Earth’s atmosphere . agree disagree
8 . Human actions can lead to a decrease in Earth’s temperature . agree disagree
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Analyzing Climate Data
Although researchers at the polar station have now concluded that global average
temperature has increased and that this is causing ice to melt, some scientists
initially disagreed that the ice was melting .
Question: Why did some scientists disagree that overall ice was decreasing?
1. Read all cards. With your partner, carefully read each Melting Ice Evidence Card .
Consider the titles and labels on each card and decide what the data can help you
explain about polar ice melting . Pay close attention to the year labels on the graph .
2. Use the Evidence Gradient to evaluate the evidence. Place the cards with
stronger evidence higher on the gradient . As you place the cards, discuss the
following questions with your partner:
• How is the evidence on each card different?
• Which evidence would be stronger or more convincing to climate
scientists? Why?
• Where do you think we should place this card? Why?
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Homework: Reading The Effects of Climate Change Article Set
Choose one article to read and annotate from The Effects of Climate Change Article
Set on the following pages . Use your active reading skills as you read and annotate
the article you choose .
Reflection Question
Use the scale below to rate how actively you read this article . Think about how much
you paid attention to your own understanding and how often you recorded your
thoughts and questions . Circle your rating .
5: I was extremely active during reading .
4: I was very active during reading .
3: I was somewhat active during reading .
2: I was not very active during reading .
1: I was not active at all during reading .
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The Effects of Climate ChangeEarth’s climate is changing. In the last hundred years, the average temperature of our planet has increased by at least 0.8 degrees Celsius (1.4 degrees Fahrenheit), and climate change scientists say that global temperature will continue to rise by at least a few more degrees in coming years. That may not sound like much, but even a small change in global temperature has a large effect on the atmosphere, biosphere, geosphere, and hydrosphere on our planet.
A warming climate changes the patterns of where living things on Earth can survive. By increasing the temperature of the planet, global
Even a small rise in global temperature can have a big impact on the entire planet..
This graph shows the change in global temperature in degrees Celsius between the years 1880 and 2009.
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warming forces many species to move, or risk dying out—and in some cases, species like the polar bear can be left with no habitat at all.
A warming climate also melts glaciers around the world, causing sea levels to rise. As the oceans take up more space, some coastal cities may end up under water. In addition, a warming climate increases the temperature of Earth’s oceans and puts more water in the atmosphere, causing more extreme weather around the globe. A wetter atmosphere means more large storms, droughts, and flooding, all of which threaten the way humans live. To learn more about the effects of global warming on Earth, choose one of the chapters that follow.
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Warming and Habitat Loss Changing global temperatures mean changing habitats—and this can be bad news for living things. A living thing’s habitat is more than just the place where it lives: habitat includes everything an animal or plant needs for its survival, such as food sources, shelter, and lots of other factors.
It’s easy to see how a warming climate trend would cause polar bears to lose their habitat. Warmer temperatures cause more ice to melt. Ice is an essential part of the polar bear habitat: the bears walk out onto ice that covers the Arctic Ocean in winter in order to reach the seals that they kill and eat. Less ice means less habitat for polar bears.
It’s harder to understand why a warming climate trend causes habitat loss for other living things, but it does. Temperature is an important part of habitat, and some species
As global temperatures rise and sea ice melts, polar bears have fewer places to live and hunt for food .
This graph compares how much of the Arctic Ocean was covered by ice in different years between 2002 and 2013. The measurements were all taken at the same time of year.
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are very sensitive to changes in temperature. For example, salmon depend on cold-water streams: young salmon die if the water in a stream becomes too warm for them.
Global warming causes habitat loss in other ways, too. For example, weather patterns change as the climate warms, making some places wetter and others drier. When habitats become wetter or drier than the animals and plants that live in them are used to, the habitats can become unlivable.
As their habitats change due to warming, some plants and animals have already begun shifting the areas where they live. Many are moving toward the poles, where temperatures are cooler. Others are moving higher up mountains. However, a mountain is only so high. Once they have reached the top of the mountain, there’s nowhere higher to go.
Young salmon need cold stream water to survive.
Pikas are small animals related to rabbits. They live in the mountains. As the climate warms, pikas are beginning to move higher up the mountain, where temperatures are cooler.
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Warming and Sea Level Rise One surprising effect of a warming global climate is rising sea levels. Sea level is the line where ocean water meets dry land: as sea level rises, more land becomes covered with water. Over the past hundred years, global sea levels have risen by 10 to 20 centimeters (4 to 8 inches). Rising sea levels can cause major problems for low-lying islands, as well as coastal cities like Miami and New York. If sea levels rise too high, some places where people now live will end up under water in the future.
How can warming cause sea levels to rise? The answer has to do with melting ice on land. Glaciers and ice sheets form when ocean water evaporates into the air, forms clouds, and falls on the land as snow. In cold areas, layers of snow build up year after year, compressing the layers below them and forming solid ice. When this ice melts, the water runs down from the land and into the ocean again. If glaciers and ice sheets melt faster than they are building up, more water ends up in the ocean. Adding water to the ocean causes sea levels to rise.
In 1910 (the photo on the left), this glacier was big enough to cover an entire valley. By 2012 (the photo on the right), the same glacier was much smaller. Much of it had melted.
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Due to rising sea levels, places where humans live now may be under water in the future.
In addition, water expands a little bit as it gets warmer. That means that warmer water takes up more space than colder water. As ocean water becomes warmer, it takes up more space and sea levels rise.
You might expect that sea levels would rise the same amount everywhere, but they don’t. Because of the shape of the land and other factors, sea levels are rising much faster in some places than in others.
This graph traces the rise of sea levels since 1993.
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Warming and Extreme Weather Even the most dire predictions of climate change predict a rise in global average temperature of only 8 degrees Fahrenheit. That doesn’t sound like much at first—it may even sound like we can look forward to nicer weather. However, rising global average temperatures lead to all kinds of weather changes...and some are not so nice. In fact, evidence shows that global warming leads to extreme weather: more severe storms, droughts, flooding, and other disasters.
As the climate warms, ocean water warms, too. Warm ocean water gives power to big storms such as hurricanes
A rise in global temperature makes severe weather events, like tornadoes, more likely.
This graph shows the number of tornadoes in the United States for each year from 1950 through 2010.
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of all kinds, including snow.
As global temperatures rise and the patterns of wind and water currents change, droughts may become more common.
Extreme weather can cause damage to people’s homes, schools, and businesses.
and typhoons. With warmer water, these storms tend to become more severe.
Warming temperatures also cause more water to evaporate, putting more moisture into the air. More moisture in the air leads to more precipitation (rain and snow). It may seem amazing that global warming can cause more snowstorms, but that’s what happens. An increase in precipitation (whether rain or snow) can lead to dangerous flooding.
While warming causes more precipitation in some areas, it can also cause droughts--a lack of precipitation. The warming climate changes patterns of wind and water currents, making some areas drier than they were before.
There’s no way to look at one particular weather event and put all the blame for it on climate change. Weather is complicated, and lots of factors combine to make events happen. However, it is clear that a warming trend makes extreme weather more likely. Some people have compared extreme weather events to home runs hit by a baseball player taking steroids. You can’t say for sure whether steroids made him hit any particular home run, but you CAN say that steroids made home runs more likely. Global warming is like putting our weather systems on steroids, making extreme events more common.
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Earth’s Changing Climate—Lesson 2
Lesson 2: Exploring Energy in the Earth System
Warm-Up
This snow fell overnight and is now starting to melt .
Why do you think the snow is melting during the day? What does energy have to do
with ice melting?
Image Credit: Shutterstock
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Earth’s Changing Climate—Lesson 2
Exploring Earth’s Changing Climate Simulation
Mission: Make the ice melt in the Earth’s Changing Climate Simulation .
1 . In Earth’s System mode, press the Reset button in the Sim before you begin .
2 . In the box below, shade in the amount of the Earth’s surface that is covered by
ice before running the Sim .
3 . In the box below, shade in the amount of the Earth’s surface that is covered by
ice after you have made some of the ice melt .
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Earth’s Changing Climate—Lesson 2
4 . What did you do to melt the ice?
5 . How did the global average temperature change when you made the ice melt?
6 . How did the energy absorbed by the surface change when you made the ice melt?
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Earth’s Changing Climate—Lesson 2
Making a Claim About Melting Ice
Part A: Group Brainstorming
1 . In groups of four, brainstorm at least three possible claims that address the
question, Why is the ice on Earth’s surface melting?
2 . Record your claims on a blank piece of paper .
Part B: Individual Claims
1 . Choose the claim you think is strongest from your group’s brainstorm and
write it below .
2 . Create a diagram that shows what you think is causing Earth’s ice to melt .
Use symbols and labels to explain what you are thinking . If there is time,
create a key that explains your symbols .
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Ice Melting Claim: Why is the ice on Earth’s surface melting?
Claim: _______________________________________________________________________________________________________________________________________________________________________________________________________________________________
Diagram (drawing) showing what you think is causing Earth’s ice to melt:
Key:
MSSCI_ECC_CU_125
Earth’s Changing Climate—Ice Melting Claim Copymaster—Lesson 1.3
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Earth’s Changing Climate—Lesson 3
Lesson 3: Testing Changes to the Atmosphere
Warm-Up
The atmosphere is about 480 km (300 miles) thick and surrounds Earth .
What do you think the atmosphere is made of?
Image Credit: Shutterstock
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Testing Nitrogen Dioxide and Carbon Dioxide in the Sim
Use the Simulation to investigate the claim that all gases affect energy absorbed by
the surface in the same way .
• One partner will test nitrogen dioxide and carbon dioxide and the other
partner will move forward and test sulfur dioxide and methane (using the
following notebook page) .
1 . Let the Sim run until the timer reaches 20 before beginning a test .
2 . Make only one change per test . When increasing, set the gas at 550 ppm; when decreasing, set the gas at 0 ppm .
3 . Run the test until the timer reaches 40 .
4 . Observe the temperature, amount of ice, and glow of absorbed energy .
5 . View the graph to observe changes in temperature, surface ice, and absorbed energy .
6 . Record your results . There is space to draw the graph on the page, Analyzing Evidence from the Sim Tests .
7 . Reset the Sim before your next test .
Answer the questions below by filling in the blanks with one of these possible
answers: increased, decreased, did not change.
When I increased nitrogen dioxide, energy absorbed by the surface ______________,
temperature ______________, and the amount of ice ______________ .
When I decreased nitrogen dioxide, energy absorbed by the surface ______________,
temperature ______________, and the amount of ice ______________ .
When I increased carbon dioxide, energy absorbed by the surface ______________,
temperature ______________, and the amount of ice ______________ .
When I decreased carbon dioxide, energy absorbed by the surface ______________,
temperature ______________, and the amount of ice ______________ .
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Testing Sulfur Dioxide and Methane in the Sim
Use the Simulation to investigate the claim that all gases affect energy absorbed by
the surface in the same way .
• One partner will test sulfur dioxide and methane and the other partner will test
nitrogen dioxide and carbon dioxide (using the previous notebook page) .
1 . Let the Sim run until the timer reaches 20 before beginning a test .
2 . Make only one change per test . When increasing, set the gas at 550 ppm; when decreasing, set the gas at 0 ppm .
3 . Run the test until the timer reaches 40 .
4 . Observe the temperature, amount of ice, and glow of absorbed energy .
5 . View the graph to observe changes in temperature, surface ice, and absorbed energy .
6 . Record your results . There is space to draw the graph on the page, Analyzing Evidence from the Sim Tests .
7 . Reset the Sim before your next test .
Answer the questions below by filling in the blanks with one of these possible answers: increased, decreased, did not change.
When I increased sulfur dioxide, energy absorbed by the surface ______________,
temperature ______________, and the amount of ice ______________ .
When I decreased sulfur dioxide, energy absorbed by the surface ______________,
temperature ______________, and the amount of ice ______________ .
When I increased methane, energy absorbed by the surface ______________,
temperature ______________, and the amount of ice ______________ .
When I decreased methane, energy absorbed by the surface ______________,
temperature ______________, and the amount of ice ______________ .
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Earth’s Changing Climate—Lesson 3
Analyzing Evidence from the Sim Tests
1 . Circle whether you now agree or disagree with the claim below and provide
evidence to support your answer .
2 . If you have time, draw the graphs from your Sim testing as part of your evidence .
• You do not need to include all four graphs . If you include graphs, describe
how they provide evidence as part of your answer . You may also annotate
the graphs .
Do you agree or disagree with the
claim, A change to any gas in the
atmosphere affects energy absorbed
by the surface in the same way.
agree disagree
What is your evidence?
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Earth’s Changing Climate—Lesson 3
Nitrogen dioxide graph
Carbon dioxide graph
Sulfur dioxide graph
Methane graph
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Earth’s Changing Climate—Lesson 3
Answering the Investigation Question
1 . With a partner, discuss using words from the Word Bank to create different
sentences that answer the Investigation Question, What kinds of changes to the
atmosphere could affect how much energy is absorbed by Earth’s surface?
2 . After you discuss some different ideas, record at least two of your sentences
below .
carbon dioxide methane temperature
energy increase decrease
absorb surface atmosphere
Word Bank
Record at least two different sentences that answer the Investigation Question .
______________________________________________________________________________
______________________________________________________________________________
______________________________________________________________________________
______________________________________________________________________________
______________________________________________________________________________
______________________________________________________________________________
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Earth’s Changing Climate—Lesson 3
Active Reading: “A Hole in Earth’s Ozone Layer”
Read the article “A Hole in Earth’s Ozone Layer” on the following notebook page and
annotate it with your questions and ideas .
As you read, continue to think about the Chapter 1 Question, Why is the ice on Earth’s
surface melting? Could changes to ozone in the atmosphere be related to climate
change?
Be sure to answer the reflection question below after you read.
Reflection Question
Use the scale below to rate how actively you read this article . Think about how much
you paid attention to your own understanding and how often you recorded your
thoughts and questions . Circle your rating .
5: I was extremely active during reading .
4: I was very active during reading .
3: I was somewhat active during reading .
2: I was not very active during reading .
1: I was not active at all during reading .
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Earth’s Changing Climate—Lesson 3
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A Hole in Earth’s Ozone LayerEarth’s atmosphere is a layer of gases that surrounds the entire planet. Each gas in the atmosphere interacts differently with energy: each gas may absorb energy, reflect it back to where it came from, or let it pass through.
One of the gases in Earth’s atmosphere is called ozone. Ozone allows some kinds of energy to pass through to Earth, but it absorbs a type of energy from the sun called UVB energy. A layer of ozone about 10 km (6 mi) above Earth’s surface surrounds the planet, keeping UVB energy from reaching Earth’s surface. This layer of ozone protects humans from the harmful effects of UVB energy, such as skin cancer.
unreveal “atmosphere”
In the 1970s, scientists noticed that the amount of ozone in the atmosphere was decreasing all over Earth, but the change was especially noticeable over Antarctica.
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Earth’s Changing Climate—Lesson 3
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Beginning in the 1970s, scientists noticed that the amount of ozone in Earth’s atmosphere was decreasing. The change was taking place because of a chemical reaction between the ozone in the atmosphere and certain types of chemicals made by humans and used in refrigerators, aerosol spray bottles, and fire extinguishers. The ozone layer was becoming especially thin over Antarctica. As the ozone layer became thinner, scientists predicted that humans would see increased rates of skin cancer and other diseases.
The hole in the ozone layer has caused an increase in the amount of UVB light that reaches Earth. This increase has had health effects for humans and other species, but it hasn’t really increased Earth’s temperature. Since global warming is caused by energy that can’t escape Earth’s atmosphere and not by extra energy reaching Earth, global climate change is not caused by the hole in the ozone layer.
There’s good news about Earth’s ozone layer: after scientists began to study the growing hole in the ozone layer and identified the chemicals that were causing it, many countries agreed to ban the use of those chemicals. Companies were required to invent refrigerators, spray bottles, and fire extinguishers that didn’t use them. Today, most people don’t use those chemicals—and the combination of these efforts are working! The hole in the ozone has shrunk since 1989, when the chemical bans went into effect. The hole in the ozone layer was caused by human actions, but is also beginning to shrink because of human actions.
The thinning ozone layer was partially caused by the chemicals used in aerosol spray cans used for hairspray and spray paint. Companies that make those products now use different chemicals to make their spray cans work.
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29
Earth’s Changing Climate—Lesson 3
absorb
to take in
absorber: retener o incorporar
atmosphere
the mixture of gases surrounding a planet
atmósfera: la mezcla de gases que rodea un planeta
carbon dioxide
a gas found in the atmosphere
dióxido de carbono: un gas que se encuentra en la atmósfera
change
when something becomes different over time
cambio: cuando algo se vuelve diferente con el tiempo
climate
general weather patterns over a long period of time
clima: condiciones atmosféricas típicas a largo plazo
climate change
changes in climate over large period of time that can be caused by natural or human activities
cambio climático: cambios en el clima durante un gran periodo de tiempo que pueden ser causados por actividades naturales o humanas
combustion
the process of burning fuels that produces carbon dioxide
combustión: el proceso de quemar combustibles que produce el dióxido de carbono
data
information collected in an investigation
datos: información recolectada en una investigación
deforestation
the process of clearing trees from land
deforestación: el proceso de quitar árboles de la tierra
energy
the ability to make things move or change
energía: la capacidad de hacer que las cosas se muevan o cambien
eruption
the sudden pushing out of something, such as lava from a volcano
erupción: la expulsión repentina de algo, como lava de un volcán
fluctuation
variations in a set of data
fluctuación: variaciones en un conjunto de datos
human activities
things people do that affect the Earth system
actividades humanas: cosas que hace la gente y que afectan al sistema Tierra
lux
a measure of how much light is present
lux: una medida de cuánta luz está presente
Earth’s Changing Climate Glossary
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30
Earth’s Changing Climate—Lesson 3
model
an object, diagram, or computer program that helps us understand something by making it simpler or easier to see
modelo: un objeto, diagrama o programa de computadora que nos ayuda a entender algo al hacerlo más simple o fácil de ver
methane
a gas found in the atmosphere
metano: un gas que se encuentra en la atmósfera
redirect
send to a new or different place
redireccionar: enviar a un lugar nuevo o diferente
reflect
to bounce off without absorbing
reflejar: rebotar sin absorber
stability
when something stays the same over time
estabilidad: cuando algo permanece igual a lo largo del tiempo
sulfur dioxide
a gas found in the atmosphere
dióxido de sulfuro: un gas que se encuentra en la atmósfera
temperature
a measure of how hot or cold something is; the higher the temperature is, the more energy it has
temperatura: una medida de que tan caliente o frío es algo; a medida que la temperatura sube, la energía también sube
the Earth system
the living and nonliving components of the Earth, including the water, land and atmosphere
el sistema Tierra: los componentes vivos y no vivos de la Tierra, incluyendo el agua, la tierra y la atmósfera
trend
overall tendency (for example, a consistent increase) in a set of data over time
tendencia: el trayectoria general (por ejemplo, un aumento consistente) en un conjunto de datos durante un período de tiempo
volcano
a mountain that has an opening in the land where gas, lava, and/or ash is pushed out
volcán: una montaña que tiene una apertura en la tierra donde el gas, lava y/o cenizas salen