More carbon dioxide is not automatically good for the planet — an idea often referred to as “global greening.” There are natural limits to how much photosynthesis plants can carry out. Plants need water and nutrients to grow, and supplies of these inputs are limited. And as carbon dioxide concentrations rise, plants’ ability to use it decreases — an effect known as carbon dioxide saturation.
For now, however, climate change has extended the growing season for trees in the Northeast by about 10-14 days. In my tree ring research, we routinely see trees putting on much more diameter growth now than in the past.
This effect is particularly evident in young trees, but we see it in old trees as well. That’s remarkable because old trees’ growth should be slowing down, not speeding up. Scientists in western states have even noted this acceleration in bristlecone pines that are over 4,000 years old — the oldest trees in the world.
Fall colors emerge when the growing season ends and trees stop photosynthesizing. The trees stop producing chlorophyll, the green pigment in their leaves, which absorbs energy from sunlight. This allows carotenoid (orange) and xanthophyll (yellow) pigments in the leaves to emerge. The leaves also produce a third pigment, anthocyanin, which creates red colors. A longer growing season may mean that fall colors emerge later — and it can also make those colors duller.
A changing mix of trees
Climate isn’t the only thing that affects fall colors. The types of tree species in a forest are an even bigger factor, and forest composition in the eastern U.S. has changed dramatically over the past century.
Notably, eastern forests today have more species such as red maple, black birch, tulip poplar and blackgum than they did in the early 20th century. These trees are shade-tolerant and typically grow in conditions that are neither extremely wet nor extremely dry. They also produce intense red and yellow displays in the fall.
This shift began in the 1930s, when federal agencies adopted policies that called for suppressing all wildfires quickly rather than letting some burn. At that time, much of the eastern U.S. was dominated by fire-adapted oak, pine and hickory. Without fires recurring once or twice a decade, these species fail to regenerate and ultimately decline, allowing more shade-tolerant, fire-sensitive trees like red maple to invade.
There is evidence that some tree species in the eastern U.S. are migrating to the north and west because of warming, increasing precipitation and fire suppression. This trend could affect fall colors as regions gain or lose particular species. In particular, studies indicate that the range of sugar maples — one of the best color-producing trees — is shifting northward into Canada.
So far it’s clear that warming has caused a delay in peak colors for much of the East, ranging from a few days in Pennsylvania to as much as two weeks in New England. It’s not yet known whether this delay is making fall colors less intense or shorter-lasting.
But I’ve observed over the past 35 years that when very warm and wet weather extends into mid- and late October, leaves typically go from green to either dull colors or directly to brown, particularly if there is a sudden frost. This year there are few intense red leaves, which suggests that warmth has interfered with anthocyanin production. Some classic red producers, such as red maple and scarlet oak, are producing yellow leaves.
Other factors could also stress eastern forests. Climate scientists project that global warming will make tropical storms and hurricanes more intense and destructive, with higher rainfall rates. These storms could knock down trees, blow leaves off those left standing and reduce fall coloration.
