Tree Rings, Climate
- Before engaging in the following activities, please read this page and the pages on each tree species.
- Use annular growth rings to compare the growth rate of all six species.
- Identify trees based on cross-sections
- Determine yearly rainfall estimates from tree-ring data
- Compare the growth characteristics of tree species
- Compare and contrast environments in which these trees grow
- Analysis of chemical composition of petrified wood
Major Trees of California
The ecology of California can be understood by dividing the state into a number of ecoregions, which contain distinct ecological communities of plants and animals in a contiguous region. The four major ecoregions of California are: desert ecoregions (such as the Mojave Desert), Mediterranean ecoregions (such as the chaparral of Southern California mountains), forested mountains (such as the Sierra Nevada, Cascades, and San Gabriels), and coastal forests (such as the Northern California Coast Ranges). Six of the largest and most important tree species in California are: Coast Live Oak (Quercus agrifolia) Coast Redwood (Sequoia sempervirens) Gray Pine (Pinus sabiniana) Incense Cedar (Calocedrus decurrens) Ponderosa Pine (Pinus ponderosa) Red Fir (Abies magnifica)
Scientists use a variety of methods to collect data about the Earth’s weather and climate. Weather stations, balloons, buoys, and satellites help researchers gather information about Earth’s current weather conditions. Scientists learn about Earth's climate in the past by studying historical records as well as clues that remain in rocks, ice, trees, corals, and fossils. These clues not only tell us how the Earth’s climate has changed, but they can also help scientists understand why these changes came about. Knowing how the Earth’s climate has changed over time can help scientists determine whether the changes that are occurring now are part of the Earth’s natural pattern or caused by human activities.
One way scientists are learning about past climate is by studying tree rings. This field of research is known as dendrochronology. Scientists can use tree rings to measure the age of a tree and learn more about the local climatic conditions the tree experienced during its lifetime.
In temperate areas, like most of the United States, trees only grow during the part of the year called the growing season. The length of this growing season depends on the climate in a particular location. During each growing season, the trunk of the tree grows thicker, producing a layer of new wood called a tree ring. It’s possible to see the boundary between one ring and the next because of differences in the color of the wood. Early in the growing season, trees grow relatively quickly and produce less-dense, paler wood. Near the end of the growing season, they produce more dense, darker wood.
Trees generally grow more during wetter growing seasons with favorable temperatures, forming wider rings. Narrow rings may be caused by stressful periods such as droughts. Although tree rings only record conditions during the growing season (in other words, not during the winter in most of the United States), droughts can build up over many months or even many years, so a lack of rain or snow in the winter can lead to poor growing conditions in the spring.
g patterns provide information about precipitation and other conditions during the time the tree was alive. Scientists can learn even more about precipitation and temperature patterns by studying certain chemicals in the wood. Modern trees can be interesting to compare with local measurements (for example, temperature and precipitation measurements from the nearest weather station). Very old trees can be even more interesting because they offer clues about what the climate was like before measurements were recorded. In most places, daily weather records have only been kept for the last 100 to 150 years. Thus, to learn about the climate hundreds to thousands of years ago, scientists need to use other sources such as trees, corals, and ice cores (layers of ice drilled out of a glacier or ice sheet—mostly in Greenland and Antarctica).
By studying tree rings and other clues in our environment, scientists have learned that there have been times when most of the planet was covered in ice, and there have also been much warmer periods. In general, climate changes prior to the start of the Industrial Revolution in the 1700s can be explained by natural causes, such as changes in solar energy and volcanic eruptions. Recent climate changes, however, cannot be explained by natural causes alone. Instead, human activities are very likely responsible. Tree rings alone cannot tell us whether human activities are responsible, but they do help by revealing patterns that scientists can investigate further. (source: NASA & EPA)
Tree rings in fossilized wood
Fossilized trees, Petrified Forest National Park, Arizona