Energy Resources

The most direct way to reduce carbon emissions is to transition from fossil fuel sources of energy to renewable sources (solar, wind, geothermal) and nuclear.  We will only get into this issue very peripherally here. As of 2026, these renewable sources of energy account for about 9% of US energy consumption, with solar producing about 4%, wind producing about 5%, and geothermal producing 0.1%. Nuclear produces about 9% of our energy. Fossil fuel sources comprise the vast majority of our energy consumed.

A stacked area chart of U.S. energy consumption by source from 1965 to 2024.
Energy consumption by source over time.
Text description of the Energy consumption by source over time image.

This image is a stacked area chart titled “Energy consumption by source, United States.” It shows U.S. primary energy consumption from approximately 1965 to 2024, measured in terawatt-hours (TWh) using the substitution method.

The horizontal axis displays years from 1965 to 2024. The vertical axis ranges from 0 to 30,000 TWh.

Each colored band represents a different energy source, stacked on top of one another to show total energy use over time. The sources listed in the legend on the right are:

  • Oil (bottom layer, blue)

  • Coal (reddish-brown)

  • Gas (green)

  • Nuclear (orange)

  • Hydropower (yellow)

  • Wind (pink)

  • Solar (bright magenta)

  • Biofuels (light green)

  • Other renewables (teal)

Total U.S. energy consumption rises steadily from the late 1960s through the early 2000s, reaching a peak slightly above 26,000 TWh around the mid-2000s. There is a noticeable drop around 2008–2009, corresponding to the financial crisis, followed by partial recovery. A sharp decline appears around 2020, followed by rebound in the early 2020s.

  • Oil remains the largest energy source throughout the entire period. It rises through the 1970s, fluctuates, peaks in the mid-2000s, declines slightly, and then stabilizes.

  • Coal increases until the early 2000s, then declines significantly after about 2008 and continues trending downward into the 2020s.

  • Natural gas grows gradually through the late 20th century and increases more strongly after 2005, eventually surpassing coal and approaching oil in magnitude.

  • Nuclear energy increases from the 1970s through the 1990s, then levels off and remains relatively stable.

  • Hydropower remains relatively stable with modest fluctuations over time.

  • Wind and solar are minimal until about 2005, then grow rapidly in the 2010s and 2020s, though they remain smaller than fossil fuels.

  • Biofuels and other renewables increase gradually in the 2000s and 2010s.

The chart shows a long-term shift in the U.S. energy mix:

  • Early dominance by oil and coal

  • Growth of natural gas

  • Decline of coal after 2008

  • Rapid expansion of wind and solar in the last decade

  • Overall energy consumption growth followed by stabilization

Credit: Energy consumption by source, United States by Max Roser from Our World in Data is licensed under CC BY 4.0. Accessed Feb. 25, 2026. 

One piece of good news in the chart is that consumption of energy produced by coal, the dirtiest source of energy, is declining.  However, you can see that the increase of energy produced from renewable sources is not increasing nearly fast enough to make a dent in the rising energy demand, you can see from the figure above that production by oil and gas have increased significantly.

Energy production and use are the most important means by which we are altering the global climate and, in turn, the changing climate will impact our energy production and consumption in a variety of ways.

Warming will be accompanied by decreases in demand for heating energy and increases in demand for cooling energy. The latter will result in significant increases in electricity use (most cooling uses electricity; heating uses a wider array of energy sources) and higher peak demand in most regions. This picture obviously changes around the country and the globe, but there has been more growth in the US in regions that are mainly cooling regions, thus exacerbating this effect. The general picture is illustrated by looking at 4 major cities in this graph that shows the degree days for heating and cooling at the present and as expected in the future under different emissions scenarios.

Bar chart comparing heating and cooling degree days in New York, Chicago, Dallas, and Los Angeles across various emissions scenarios.

Four major cities in this graph show the degree days for heating and cooling at the present and as expected in the future under different emissions scenarios

The graph shows the percentage contribution of different sectors to global carbon emissions. The x-axis lists the sectors, while the y-axis represents the percentage (0% to 40%). The sectors and their contributions are: Electricity and Heat Production (30%, gray), Transportation (20%, blue), Industry (18%, orange), Residential (10%, green), Agriculture (8%, yellow), Commercial and Public Services (6%, purple), and Other Energy (8%, red). The graph visually emphasizes that Electricity and Heat Production is the largest contributor to carbon emissions.

  • Graph Overview
    • Title: Global Carbon Emissions by Sector (2016)
    • Type: Bar graph
  • Axes
    • X-axis: Sectors
    • Y-axis: Percentage (0% to 40%)
  • Sectors and Contributions
    • Electricity and Heat Production: 30% (gray)
    • Transportation: 20% (blue)
    • Industry: 18% (orange)
    • Residential: 10% (green)
    • Agriculture: 8% (yellow)
    • Commercial and Public Services: 6% (purple)
    • Other Energy: 8% (red)
  • Visual Emphasis
    • Electricity and Heat Production: Largest bar, highlighting its dominance
Credit: David Bice © Penn State University is licensed under CC BY-NC-SA 4.0

One heating degree day is one day where the outside temperature is 1°F below 65°F; two cooling degree days is either one day at a temperature of 67°F or two days at 66°F. If you then sum these up for a whole year, you have the data shown in this figure (Recent History bars). The colder cities like Chicago and New York have larger heating degree day sums than cooling degree day sums.

Energy production is likely to be constrained by rising temperatures and limited water supplies in many regions. Power plants are the second biggest user of surface water (after irrigation) and the hotter it is, the more water is needed to cool the plants. At the same time, as the water warms, you need more of it to accomplish the same cooling job. A powerful example of this effect comes from the French heat wave of 2003, during which a number of nuclear power plants had to halt production because the cooling water was not cool enough to safely continue generating electricity.

Energy production and delivery systems are exposed to sea-level rise and extreme weather events in vulnerable regions. A good example of this comes from Port Fourchon, Louisiana, which supports 75% of deepwater oil and gas production in the Gulf of Mexico, and its role in supporting oil production in the region is increasing. The Louisiana Offshore Oil Port, located about 20 miles offshore, receives 1.3 million barrels of oil per day and transfers it to refineries, accounting for 50% of our nation's refining capacity, making this one of the most important components of our energy production system. One road, Louisiana Highway 1, connects Port Fourchon with the nation, and it is increasingly vulnerable to flooding during storms due to the combined effects of sea level rise and ground subsidence. Louisiana is currently upgrading Highway 1, elevating it above the 500-year flood level in order to prolong its viability.

Climate change is also likely to affect some hydropower production in regions subject to changing patterns of precipitation or snowmelt.

How can we adapt to these coming changes? Part of the solution is to identify vulnerable features of our energy production system (such as Port Fourchon) and then safeguard them from the expected consequences of continued warming. Another big part of the adaptive strategy is to reduce our consumption of energy by increasing efficiencies in transportation (which we are already doing), home appliances, and buildings. New York City and Chicago have both undertaken massive programs to minimize the heat absorbed by their cities by planting trees and installing reflective or green roofs on buildings. Trees and green roofs cool by evapotranspiration, and the effect can be significant. These steps will reduce the cooling demands in these cities. We can also reduce the demand on power plants by more distributed, small-scale energy production that is carbon neutral. This is happening in a big way in many parts of Europe, where fields of solar panels have been springing up in farmers' fields — they are growing energy, attracted by strong support from the state-run utilities responsible for electricity.