Agniverse

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Earth's Systems

Atmosphere

Hydrosphere

Cryosphere

Geosphere

Biosphere

Atmosphere

The thin layer made up of a mixture of gases and particles suspended in the air that surround the Earth (78% N2, 21% oxygen, 0.9% argon, and 0.1% other gases).
There are five main layers that make up the atmosphere:
  • 1. Troposphere: The lowest layer where weather occurs and where we live. It contains about 75% of the atmosphere’s mass.

  • 3. Stratosphere: Contains the ozone layer, which absorbs and scatters ultraviolet solar radiation.

  • 3. Mesosphere: The layer where most meteors burn up upon entering the atmosphere.

  • 4. Thermosphere: A layer with very thin air, where the auroras occur and the International Space Station orbits.

  • 5. Exosphere: The outermost layer, where the atmosphere thins out into space.

Source: https://www.nasa.gov/general/what-is-earths-atmosphere

Hydrosphere

A sphere that includes the liquid ocean, inland water bodies and groundwater.

Hydrosphere covers 70% of the Earth’s surface.

Hydrosphere is necessary for sustaining life on Earth.

The Hydrosphere is a crucial part for the Water Cycle, includes processes like evaporation, condensation, precipitation etc.

Oceans absorb and store solar energy, distribute heat around the globe through currents and influence weather patterns.

Source: https://mynasadata.larc.nasa.gov/basic-page/about-hydrosphere

Cryosphere

A subset of the Hydrosphere that consists of frozen water. (Snow and Ice)

The Cryosphere plays a critical role in regulating climate and sea levels.

Around three-quarters of the world’s fresh water is stored in the Cryosphere, primarily in glaciers and ice caps.

The Cryosphere helps regulate Earth’s climate by reflecting incoming solar radiation back into space, a process known as the albedo effect.

Melting ice from the cryosphere contributes to sea level rise, which can impact coastal ecosystems and human settlements.

Source: https://mynasadata.larc.nasa.gov/basic-page/about-cryosphere

Geosphere

A sphere that includes the solid Earth; the core, mantle, crust and soil layers.

94% of the solid Earth is made up of the following elements: oxygen, iron, silicon, and magnesium.

The movement of the tectonic plates causes earthquakes, volcanic eruptions and the formation of mountains.

The geosphere is a source of essential natural resources, including minerals, fossil fuels and soil, which are crucial for human activities and ecosystems.

Source: https://mynasadata.larc.nasa.gov/basic-page/about-geosphere

Biosphere

The Biosphere includes all life on Earth including life living on the Earth's Geosphere and in Hydrosphere, including humans and all organic matter that has not yet decomposed.

The Biosphere functions as Earth’s life support system, regulating atmospheric composition, soil health, and the hydrological cycle.

It is home to a vast diversity of life forms, from microorganisms to plants and animals. Biodiversity within the biosphere is crucial for ecosystem stability and resilience.

The biosphere helps regulate Earth’s climate by influencing the carbon cycle and other biogeochemical cycles.

The biosphere interacts with the atmosphere, hydrosphere, and geosphere, creating a complex web of interdependencies that sustain life on Earth.

Source: https://mynasadata.larc.nasa.gov/basic-page/about-biosphere

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The temperature

The Water level

The glacier level

The lava level

The trees level

Our Earth is a beautifully interconnected system
shaped by even our smallest actions

Let's Explore

Atmosphere

OCO-2 and Keelling Curve: Trends in global atmospheric Carbon Dioxide (CO2)
Trends in atmospheric Methane (CH4)

How does it affect other systems?

Hydrosphere

Atmospheric changes lead to evaporation, changing rainfall patterns & ocean temperatures.

Biosphere

Warmer or polluted air affects plant growth, animal migration, and ecosystem stability.

Cryosphere

Higher temperatures result in the melting of glaciers, sea ice, and permafrost.

Geosphere

Changes in temperature can accelerate erosion and alter soil stability.

Natural Causes: Volcanic eruptions, solar radiation, and variations in Earth's orbit can change temperature, air pressure, and gas composition.

Human Impact: Industrial emissions (e.g., CO₂, methane), deforestation, and pollution contribute to changes like global warming and ozone depletion.

How can we prevent the effect?

Tree Plantation and Reforestation:

Benefits: Trees absorb CO2, regulate the water cycle, reduce air pollution, prevent soil erosion, and provide habitats for wildlife.

Action: Large-scale reforestation programs and protection of existing forests can significantly help balance carbon levels and enhance biodiversity.

Promoting Renewable Energy:

Benefits: Shifting from fossil fuels to renewable energy sources like solar, wind, geothermal, and hydroelectric power reduces greenhouse gas emissions and dependence on non-renewable resources.

Action: Governments, businesses, and individuals can invest in renewable energy infrastructure and technologies to reduce the carbon footprint.

Sustainable agriculture:

Benefits: Practices like crop rotation, agroforestry, organic farming, and reducing chemical inputs can enhance soil health, reduce emissions, and minimize deforestation.

Action: Supporting local, sustainable farming practices and reducing food waste can lower the ecological footprint of agriculture.

Hydrosphere

Water system information and controls...

Cryosphere

Ice system information and controls...

Geosphere

Geological system information and controls...

Biosphere

Biological system information and controls...

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Climate Change

What is climate?

According to NASA , climate refers to the long-term average of weather patterns that define Earth’s local, regional, and global climates. These patterns include temperature, precipitation, and other weather variables averaged over several decades.Climate change increases the frequency and severity of natural hazards like heatwaves, floods, droughts, and storms by altering temperatures, precipitation patterns, and sea levels.

Climate Change Elements

Carbon Dioxide (CO₂)

The most significant greenhouse gas from human activities, accounting for about 76% of total greenhouse gas emissions.

Current Level: ~420 ppm (parts per million)

Pre-industrial Level: ~280 ppm

Rate of Increase: About 2.5 ppm per year

Main Sources:
  • Fossil fuel combustion (coal, oil, gas)
  • Deforestation and land use changes
  • Industrial processes (cement production)
  • Transportation and aviation
Impact: CO₂ traps heat in the atmosphere, contributing to global warming and climate change.

Methane (CH₄)

A potent greenhouse gas that is 25 times more effective at trapping heat than CO₂ over a 100-year period.

Current Level: ~1,900 ppb (parts per billion)

Pre-industrial Level: ~700 ppb

Global Warming Potential: 25x CO₂

Main Sources:
  • Agriculture (livestock, rice cultivation)
  • Natural gas production and distribution
  • Landfills and waste treatment
  • Coal mining
  • Natural wetlands
Lifetime: Methane has a shorter atmospheric lifetime (~9 years) than CO₂, but is much more potent.

Nitrous Oxide (N₂O)

A powerful greenhouse gas with a global warming potential nearly 300 times greater than CO₂.

Current Level: ~335 ppb (parts per billion)

Pre-industrial Level: ~270 ppb

Global Warming Potential: 298x CO₂

Atmospheric Lifetime: ~114 years

Main Sources:
  • Agricultural practices (fertilizer use)
  • Fossil fuel combustion
  • Industrial activities
  • Natural soil processes
  • Ocean processes
Additional Impact: N₂O also contributes to stratospheric ozone depletion.

Chlorofluorocarbons (CFCs)

Synthetic compounds once widely used in refrigeration and aerosols, now largely phased out due to the Montreal Protocol.

Current Status: Declining due to international regulations

Global Warming Potential: 4,750-14,400x CO₂

Atmospheric Lifetime: 45-1,700 years

Historical Uses:
  • Refrigerants and air conditioning
  • Aerosol propellants
  • Foam blowing agents
  • Industrial solvents
Environmental Impact: CFCs not only warm the planet but also deplete the ozone layer, creating the "ozone hole."

Water Vapor (H₂O)

The most abundant greenhouse gas in the atmosphere, playing a crucial role in Earth's climate system as both a greenhouse gas and climate feedback mechanism.

Atmospheric Concentration: Highly variable (0.001% - 5%)

Average Residence Time: ~10 days

Climate Feedback: Positive feedback amplifies warming

Key Characteristics:
  • Natural component of the water cycle
  • Concentrations controlled by temperature
  • Forms clouds that both cool and warm
  • Amplifies warming from other gases
  • Cannot be directly controlled by humans
Feedback Loop: As temperatures rise, more water evaporates, creating more water vapor, which traps more heat.

Global Temperature

Global temperature anomaly is how much warmer or colder than the long-term average a unit of time something is (like how much warmer than average the most recent year was globally).

The 10 most recent years are the warmest years on record.

Time Series: 1884 to 2022

Data source: NASA/GISS
Credit: NASA's Scientific Visualization Studio

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1884

2022

The animation on the right shows the change in global surface temperatures. Dark blue shows areas cooler than average. Dark red shows areas warmer than average. Short-term variations are smoothed out using a 5-year running average to make trends more visible in this map.

Sea Level

Sea level refers to the average height of the ocean’s surface.

The Earth’s seas are rising at a higher rate than they have in the past. This change is a direct result of a changing climate.

Increased Greenhouse Gases Lead to Global Sea Level Rise

This animation shows the rise in global mean sea level from 1993 to 2023 based on data from a series of five international satellites. The spike in sea level from 2022 to 2023 is mostly a consequence of climate change and the development of El Niño conditions in the Pacific Ocean.Credit: NASA's Scientific Visualization Studio.

What Couses Global Sea Level Rise?

  • Greenhouse gases added to the atmosphere by human activities are warming the planet.
  • Global sea level is rising mainly from ocean warming and melting land ice due to climate change.
  • Global sea level is rising faster today than it was 100 years ago.
  • For over 100 years, humans have burned coal, gas, and oil to produce energy. Burning these fossil fuels releases greenhouse gases into the air.
  • Around 90% of the added heat from greenhouse gases is being absorbed by the ocean, warming it up.Currently, about one third (around 33%) of global sea level rise is because of ocean warming.
  • As Earth heats up, it melts the land ice, including the Greenland and Antarctic Ice Sheets and other mountain glaciers. The water then flows into the ocean which raises sea levels. Around 66% of global sea level rise is because of melting land ice.

Ocean Warming

The Ocean's Role as Earth's Heat Sink

The ocean has absorbed about 90% of the excess heat trapped by greenhouse gases, making it a crucial indicator of climate change.

Heat Absorption: ~93% of excess heat goes into oceans

Temperature Rise: Upper 2000m warmed by ~0.6°C since 1969

Rate of Warming: Accelerating, especially since 1990s

Impacts of Ocean Warming:
  • Thermal expansion contributing to sea level rise
  • Changes in ocean circulation patterns
  • Marine ecosystem disruption
  • Coral bleaching events
  • Altered weather patterns globally
  • Reduced oxygen levels in seawater

Ice Sheets

Greenland Ice Sheet

The world's second-largest ice sheet, covering ~80% of Greenland's surface.

Ice Loss Rate: ~280 billion tons per year

Sea Level Potential: ~7.4 meters if completely melted

Current Contribution: ~0.7mm/year to sea level rise

Antarctic Ice Sheet

The world's largest ice sheet, containing ~90% of Earth's fresh water.

Ice Loss Rate: ~150 billion tons per year

Sea Level Potential: ~58.3 meters if completely melted

Most Vulnerable: West Antarctic Ice Sheet

Key Processes:
Surface Melting

Direct melting from warm air temperatures

Basal Melting

Melting from underneath by warm ocean water

Calving

Ice breaking off into icebergs at the edges

Albedo Effect

Less ice means less sunlight reflection

Arctic Sea Ice

Current Trends

Arctic sea ice is declining at an unprecedented rate, with significant implications for global climate.

Decline Rate: ~13% per decade since 1979

Minimum Extent: Occurs in September each year

Thickness Loss: ~66% thinner than in 1958

Climate Impacts
  • Reduced albedo (ice reflects sunlight)
  • Increased heat absorption by dark ocean
  • Disrupted polar weather patterns
  • Habitat loss for Arctic wildlife
  • Changes in ocean circulation
  • Potential for Arctic shipping routes
Feedback Loops:
Ice-Albedo Feedback:

Less ice → More dark ocean surface → More heat absorption → More warming → Even less ice formation

Summer Ice Loss

Arctic could be ice-free in summer by 2050

Global Impact

Arctic warming affects weather worldwide

Natural Hazards

What Natural Hazard Means?

Natural hazards are extreme environmental events that have the potential to cause significant harm to human societies and the environment. These events can lead to loss of life, injury, property damage, and disruption of human activities

Climate change increases the frequency and severity of natural hazards like heatwaves, floods, droughts, and storms by altering temperatures, precipitation patterns, and sea levels.

What is Drought?

Drought is a prolonged period of abnormally low rainfall, leading to water shortages, low soil moisture, and stressed vegetation. It affects agriculture, ecosystems, and water supplies.

The National Weather Service office of the NOAA defines drought as "a deficiency of moisture that results in adverse impacts on people, animals, or vegetation over a sizeable area".

Categories

There are three major categories of drought based on where in the water cycle the moisture deficit occurs:

Meteorological
  • Meteorological Drought occurs when there is a prolonged time with less than average precipitation.
  • Usually precedes the other kinds of drought.
  • As the drought persists, the conditions surrounding it gradually worsen and its impact on the local population gradually increases.
Hydrological
  • Hydrological drought is brought about when the water reserves available in sources fall below a locally significant threshold.
  • Tends to show up more slowly because it involves stored water that is used but not replenished.
Agricultural
  • Agricultural or ecological droughts affect crop production or ecosystems in general
  • Also arise independently from any change in precipitation levels when either increased irrigation or soil conditions and erosion triggered by poorly planned agricultural endeavors cause a shortfall in water available to the crops.

What Causes Drought?

Drought is a recurring feature of the climate in most parts of the world, becoming more extreme and less predictable due to climate change.

General Precipitation Deficiency
Dry season
Climate change
El Niño–Southern Oscillation (ENSO)
Erosion and human activities

Impacts

Droughts are the second-most costly weather events after hurricanes. Unlike with sudden weather events such as hurricanes, tornadoes, and thunderstorms, it is often difficult to pinpoint when a drought has started or when it has ended. The longer a drought lasts, the greater the harmful effects it has on people.

NASA | Brazil’s Extreme Drought Seen From Space

NASA | Brazil’s Extreme Drought Seen From Space

Environmental Impacts
  • Lower surface and subterranean water-levels
  • Lower flow-levels (with a decrease below the minimum leading to direct danger for amphibian life)
  • Increased pollution of surface water
  • The drying out of wetlands, more and larger wildfires, higher deflation intensity
  • Loss of biodiversity, worse health of trees and the appearance of pests and dendroid diseases
Economic Impacts
  • Lower agricultural, forests, game and fishing output
  • Higher food-production costs, lower energy-production levels in hydro plants
  • Losses caused by depleted water tourism and transport revenue
  • Disruption of water supplies for municipal economies.
Agricultural Impacts
  • Land degradation and loss of soil moisture, resulting in the destruction of cropland productivity
  • Poor germination and impaired seedling development for plants.
  • The reduction in crop yield results from a decrease in photosynthetic rate
Social and health impacts
  • Crop failure, food crisis, famine, malnutrition, and poverty, which lead to loss of life and mass migration of people.
  • Limitations of water supplies, increased water pollution levels, high food-costs, stress caused by failed harvests.
  • Social unrest
  • War over natural resources, including water and food can be a devastating consequence.
Loss of Fertile Soils
  • Wind erosion is much more severe in arid areas and during times of drought.
  • Soil erosion
  • Desertification
  • Loss of Vegetation
  • Reduces soil moisture
Regions Particularly Affected
  • Amazon Basin: In 2005, parts of the Amazon basin experienced the worst drought in 100 years.
  • Australia: The 1997–2009 Millennium Drought in Australia led to a water supply crisis across much of the country.
  • Himalayan River Basins: Approximately 2.4 billion people live in the drainage basin of the Himalayan rivers.[93] India, China, Pakistan, Bangladesh, Nepal and Myanmar could experience floods followed by droughts in coming decades.

Protection

Water Conservation: Implementing water-saving techniques in agriculture, industry, and households to reduce water usage.

Sustainable Agriculture: Using drought-resistant crops and efficient irrigation systems to minimize water consumption.

Forest and Land Management: Protecting and restoring forests and wetlands to maintain natural water cycles and prevent soil erosion.

Mitigation

Drought Monitoring and Early Warning Systems: The GRACE-FO (Gravity Recovery and Climate Experiment Follow-On) mission provides data for assessing changes in groundwater levels, and NASA’s Drought Monitor helps track the intensity and duration of droughts.

Infrastructure Improvements: Building and maintaining reservoirs, dams, and water distribution systems to store and manage water more effectively.

Policy and Planning: Developing and enforcing policies that promote sustainable water use and land management practices.

Relief

Financial Assistance: Providing emergency funds and loans to farmers, businesses, and communities affected by drought.

Technical Support: Offering guidance and resources to implement drought-resistant practices and technologies.

Community Support Programs: Establishing programs to support affected communities, including food and water distribution, and mental health services.

Flood

Flood Satellite

Floods are among the most common and devastating natural hazards, occurring when water overflows onto land that is usually dry. They can result from heavy rainfall, river overflow, storm surges, or dam breaks.

  • Impacts: Loss of life, property damage, waterborne diseases, and disruption of infrastructure.
  • Climate Link: Climate change increases the frequency and intensity of extreme rainfall events, raising flood risks worldwide.
Watch: How Floods Work (YouTube)
NASA: What Causes Floods?

Wildfire

Wildfire

Wildfires are uncontrolled fires that rapidly spread across vegetation, forests, and grasslands. They are fueled by dry conditions, heatwaves, and strong winds.

  • Impacts: Destruction of ecosystems, air pollution, property loss, and threats to human health.
  • Climate Link: Rising temperatures and prolonged droughts due to climate change are increasing wildfire frequency and severity.
Watch: How Wildfires Spread (YouTube)
NASA: Wildfire Season

Cyclone

Cyclone Cross Section Hurricane Florence from ISS

Cyclones (also called hurricanes or typhoons) are powerful rotating storm systems characterized by strong winds, heavy rain, and storm surges. They form over warm ocean waters and can cause widespread destruction when they make landfall.

  • Impacts: Coastal flooding, wind damage, landslides, and loss of life.
  • Climate Link: Warmer ocean temperatures are making cyclones more intense and increasing the risk of extreme weather events.
Watch: How Cyclones Form (YouTube)
NASA: Cyclones & Climate Change

COMING SOON...

COMING SOON...

COMING SOON...

COMING SOON...

Influences of Climate Change

What is Air Quality?

Air quality is a measure of the pollution level in the air. Monitoring air quality is important because polluted air can be bad for human health and the environment.

Image Credit: NOAA

Sources of Air Pollution

Pollutants are formed from both natural and human sources.

Anthropogenic Sources
  • Fuel combustion sources (such as electric utilities and boilers)
  • Industrial processes (such as metal smelters, petroleum refineries, cement kilns and dry cleaners)
  • Highway vehicles
  • Other mobile sources (such as recreational and construction equipment, marine vessels, aircraft and locomotives)
Natural Sources
  • Pollen
  • Volcanoes (release of sulfates)
  • Fires (release of organic/black carbon)
  • Desert dust
  • Sea salt

6 Criteria Pollutants

Carbon Monoxide
Lead
Nitrogen Dioxide
Ozone
Particulate Matter
Sulfur Dioxide

Trends in Air Quality

While air quality can exceed standards in specific locations on specific days, the overall air quality in the U.S. has improved since 1990.

Air Quality index

The overall air quality in an area is measured using the U.S. Environmental Protection Agency's Air Quality Index, or AQI. AQI is a unitless number, from 0 to 500, that communicates the health risk caused by the amount of pollution in the air. Higher AQI values relate to increased health risk.

Air Sensors: Measurements and Your Health

Health Effects of Air Pollution

Short and long-term exposure to air pollution has been associated with a wide range of human health effects including increased respiratory symptoms, and heart or lung diseases. Hazardous (or toxic) air pollutants may cause cancer or other serious health effects.

Environmental Effects of Air Pollution

Harm to Animals and Plants

Air pollution can affect many parts of the environment. It can cause damage to plants and the respiratory systems of animals. It can also cause damage to entire habitats, water, or food sources that plants and animals need to survive.

Acid Rain

Acid rain forms when sulfur dioxide and nitrogen dioxide mix with water droplets in the atmosphere to make sulfuric acid and nitric acid. When the pollutants fall to the surface as acid rain, they can acidify the water and soil environments, damage vegetation, and even damage buildings and outdoor structures.

Haze

Haze is caused when sunlight encounters tiny pollution particles in the air. Haze obscures the clarity, color, texture, and form of what we see.

Ozone Depletion

Depending on where ozone resides, it can protect or harm life on Earth. Most ozone resides in the stratosphere (a layer of the atmosphere between 10 and 31 miles above us), where it acts as a shield to protect Earth's surface from the sun's harmful ultraviolet radiation. This portion of ozone is ofter referred to as "good ozone." In the troposphere (the atmospheric layer from the surface up to about 10 miles), ozone is a harmful pollutant that causes damage to lung tissue and plants. This type of ozone is often referred to as "bad ozone". Scientists have found that the "bad" tropospheric ozone is increasing in the air we breathe, and the "good" stratospheric ozone is decreasing in our protective ozone layer.

Climate Change Impact on Biodiversity

Forest Biodiversity

Climate change is fundamentally altering ecosystems worldwide, threatening the delicate balance that supports Earth's incredible biodiversity.

  • Species Migration: Changing temperatures force species to migrate to new habitats or face extinction.
  • Habitat Loss: Rising sea levels, droughts, and extreme weather destroy critical ecosystems.
  • Food Chain Disruption: Changes in timing of seasons affect pollination, breeding, and feeding cycles.
Watch: Climate Change & Wildlife (YouTube)
NASA: Climate Effects on Ecosystems
Polar Ecosystems

Arctic and Antarctic regions are warming twice as fast as the global average, threatening polar bears, penguins, and entire ice-dependent ecosystems.

Coral Reefs

Ocean acidification and warming waters cause coral bleaching, affecting 25% of marine species that depend on coral reefs.

Climate Change Impact on Agriculture

Agriculture Field

Agriculture is highly vulnerable to climate change, with shifting weather patterns, extreme events, and rising temperatures affecting crop yields worldwide.

  • Crop Yields: Heat stress and changing precipitation patterns reduce yields of major crops like wheat, rice, and corn.
  • Water Scarcity: Droughts and changing rainfall patterns threaten irrigation systems and water availability.
  • Pest & Disease: Warmer temperatures expand the range of agricultural pests and diseases.
Watch: Climate Change & Food Security (YouTube)
NASA: Agriculture & Climate Data
Adaptation Strategies

Farmers are developing drought-resistant crops, precision agriculture, and sustainable farming practices to adapt to changing conditions.

Food Security

Climate change threatens global food security, potentially affecting 2 billion people by 2050 through reduced crop productivity.

Climate Change Impact on Water Resources

Water Resources

Climate change dramatically alters the global water cycle, affecting freshwater availability, quality, and distribution patterns worldwide.

  • Water Scarcity: Changing precipitation patterns create droughts in some regions while causing floods in others.
  • Glacier Melting: Shrinking glaciers threaten water supplies for billions of people who depend on glacial meltwater.
  • Groundwater Depletion: Increased demand and reduced recharge rates deplete vital aquifers.
Watch: Climate Change & Water Cycle (YouTube)
NASA: Water & Climate Change
Extreme Events

More frequent and intense droughts, floods, and storms disrupt water infrastructure and contaminate water supplies.

Water Quality

Higher temperatures promote algal blooms and bacterial growth, while floods increase water contamination risks.

Climate Change Impact on Sea Levels

Rising Sea Levels

Rising sea levels are one of the most visible and consequential impacts of climate change, threatening coastal communities and ecosystems worldwide.

  • Thermal Expansion: Warming oceans expand, contributing ~50% of current sea level rise.
  • Ice Sheet Melting: Greenland and Antarctic ice loss accelerates sea level rise globally.
  • Coastal Flooding: Higher sea levels increase frequency and severity of coastal flooding events.
Watch: Sea Level Rise Explained (YouTube)
NASA: Sea Level Rise Data
Current Rate

Sea levels are rising at 3.3mm per year, with the rate accelerating due to increasing ice sheet contributions.

Future Projections

Sea levels could rise 0.3-1.1 meters by 2100, threatening 630 million people living in coastal areas.

Climate Change & Renewable Energy

Renewable Energy

Renewable energy is crucial for mitigating climate change, but climate change also affects renewable energy production and distribution systems.

  • Solar Energy: Extreme heat can reduce solar panel efficiency, while dust storms affect energy production.
  • Wind Energy: Changing wind patterns affect turbine placement and energy generation potential.
  • Hydropower: Droughts and changing precipitation patterns affect water availability for hydroelectric generation.
Watch: Renewable Energy Solutions (YouTube)
NASA: Renewable Energy & Climate
Adaptation Needs

Renewable energy infrastructure must be designed to withstand extreme weather events and changing climate conditions.

Opportunities

Climate change creates new opportunities for renewable energy in regions with increased sun exposure or changing wind patterns.

Prevention & Mitigation

Reduce Greenhouse Gas Emissions

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Reduce, Reuse and Recycle

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Support Reforestation and Afforestation

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Create Awareness

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NASA's FIRMS

Providing Active Fire Data for Near Real-Time Monitoring and Applications

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Earth System Data Explorer

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Global Warming

Global warming is the long-term heating of Earth’s surface observed since the pre-industrial period (between 1850 and 1900) due to human activities, primarily fossil fuel burning, which increases heat-trapping greenhouse gas levels in Earth’s atmosphere. This term is not interchangeable with the term "climate change."

https://science.nasa.gov/climate-change/what-is-climate-change

The Ocean Is Getting Warmer

The ocean has absorbed much of this increased heat, with the top 100 meters (about 328 feet) of ocean showing warming of 0.67 degrees Fahrenheit (0.33 degrees Celsius) since 1969.6 Earth stores 90% of the extra energy in the ocean.Covering more than 70% of Earth’s surface, our global ocean has a very high heat capacity. It has absorbed 90% of the warming that has occurred in recent decades due to increasing greenhouse gases

https://science.nasa.gov/climate-change/faq/is-the-ocean-continuing-to-warm

Global Temperature Is Rising

The planet's average surface temperature has risen about 2 degrees Fahrenheit (1 degrees Celsius) since the late 19th century, a change driven largely by increased carbon dioxide emissions into the atmosphere and other human activities.4 Most of the warming occurred in the past 40 years, with the seven most recent years being the warmest. The years 2016 and 2020 are tied for the warmest year on record.

https://climate.nasa.gov/vital-signs/global-temperature/?intent=121

Longer Wildfire Season

TWarming temperatures have extended and intensified wildfire season in the West, where long-term drought in the region has heightened the risk of fires. Scientists estimate that human-caused climate change has already doubled the area of forest burned in recent decades. By around 2050, the amount of land consumed by wildfires in Western states is projected to further increase by two to six times. Even in traditionally rainy regions like the Southeast, wildfires are projected to increase by about 30%.

https://science.nasa.gov/earth/climate-change/study-fire-seasons-getting-longer-more-frequent

What is drought?

Around the world, droughts are becoming increasingly common due to rising global temperatures—and have serious impacts, leading to crop failures, famine and malnutrition. East Africa, for example, is facing its worst drought in years, affecting 40 million people. Many are facing near-famine and malnutrition because of the drought’s impact on food supplies.

https://www.nasa.gov/centers-and-facilities/goddard/warming-makes-droughts-extreme-wet-events-more-frequent-intense

What Causes Floods?

A flood is a water body that occupies ground that is ordinarily dry. Floods are widespread natural phenomena that can affect millions of people worldwide. Drinking water can also be polluted by flooding and contribute to illnesses.

A flood happens when water from a river , lake , or ocean overflows onto the land around it . Too much rain or melting snow are the main causes of floods

https://science.nasa.gov/science-research/earth-science/22jul_floods

What are the Effects of Flood?

When rain falls, the soil usually soaks it up like a sponge. But when the soil can’t soak up any more water., it will send extra water into a river. THis happens a lot during the winter because frozen soil can’t soak up water. Floods often happen when the warm weather of spring melts snow before the ground has time to thaw.

https://science.nasa.gov/science-research/earth-science/22jul_floods

What cyclone means?

A storm or system of winds that rotates about a center of low atmospheric pressure, advances at a speed of 20 to 30 miles (30 to 50 kilometers) an hour, and often brings a great deal of rain.

A cyclone forms in an area of low pressure. This area of low pressure draws in surrounding winds. As the Earth rotates, it creates forces that cause the winds to swirl around the low pressure. This helps the cyclone start to spin.

https://science.nasa.gov/earth/climate-change/what-climate-change-means-for-glaciers-storms-fires-clouds-and-more

What Causes Storm Surge?

As storm surge, the temporary rise in sea level beneath a storm, becomes dangerous when the storm, typically a hurricane or other tropical storm , reaches land. The water is unable to escape anywhere but onto land as the storm moves toward the shore, which causes flooding along the coast and other types of hurricane damage.

https://science.nasa.gov/earth/climate-change/a-force-of-nature-hurricanes-in-a-changing-climate

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NASA celebrated the 44th anniversary of Earth Day with a variety of live and online activities April 21-27 to engage the public in the agency's mission to better understand and protect our home planet.

Source: https://science.nasa.gov/earth/earth-day

With Earth Day coming up on April 22, the Global Precipitation Measurement (GPM) mission is hosting a free webinar to describe how and why NASA missions—and the data from these missions—can help us better understand and protect our home planet's climate and ecosystems.

Source: https://www.earthdata.nasa.gov/learn/webinars-and-tutorials

NASA's Earth Observing System Data and Information System (EOSDIS) is a key core capability in NASA’s Earth Science Data Systems Program. It provides end-to-end capabilities for managing various sources – satellites, aircraft, field measurements, and various other programs.

Source: https://www.earthdata.nasa.gov/eosdis/daacs

An upbeat invitation to "Take AIM at Climate Change" - with "AIM" standing for Adapt, Innovate, Mitigate. The lyrics are based on the latest science of Earth's changing climate, with the music a mix of rap and pop.

Source: https://www.nasa.gov/stem-content/take-aim-at-climate-change-music-video/

Discover what NASA’s Earth data sounds like when it’s turned into music. With each passing Earth Day, the drums get louder. Every sound and instrument tell a story.

Source: https://youtu.be/UU-wmSEPiqw

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