New study: Fast Transit of Water from Soil to Atmosphere Through Plants
New YorkA recent study led by scientists from Chapman University, including Dr. Andrew Felton and Dr. Gregory Goldsmith, offers a new understanding of how water rapidly moves back to the atmosphere through Earth's plants. The research, published in Nature Water, highlights the role of plants in the global water cycle.
Key findings include:
- Earth's plants store about 786 cubic kilometers of water, which represents only 0.002% of the total freshwater on Earth.
- Water transit time, or the time it takes for water to move through plants, is one of the quickest parts of the water cycle, ranging from five days in croplands to 18 days in evergreen needleleaf forests.
- The global median for water transit through plants is about 8.1 days.
- In comparison, water in lakes takes about 17 years to move through, while glaciers take around 1600 years.
This study utilized data from NASA’s SMAP satellite mission to estimate water storage in plants, which contributed to identifying the speed at which water transfers back to the atmosphere through vegetation. Croplands, grasslands, and savannas were found to exhibit particularly fast transit times, with water moving through croplands in under a day during the peak growing season.
A significant observation is that rapid water cycling in croplands could lead to more frequent heavy rainfalls, indicating that changes in land use may speed up the global water cycle. This research emphasizes that plants play a pivotal yet often overlooked role in this cycle. The results also suggest that events like deforestation, droughts, and wildfires can drastically alter water transit times, impacting the overall speed of the water cycle on a global scale.
Understanding the quick transit of water through plants is crucial for predicting how future land use and climate changes may affect the environment.
Transit Time Insights
The study highlights how quickly water moves through plants, an area often overlooked in understanding the water cycle. The research shows that water transit time through plants is surprisingly short, much faster than through lakes or glaciers. These insights help us understand how changes in our environment, like land use and climate, affect the water cycle.
The findings suggest several implications:
- Plants play a crucial role in the water cycle, acting as fast pathways for water to return to the atmosphere.
- Land use changes, such as converting forests to croplands, may speed up water cycling, affecting local weather patterns.
- The rapid transit in croplands can lead to more heavy rain events, as water returns to the atmosphere quickly.
Water's journey through plants is much faster compared to other parts of the water cycle. The study finds that in croplands, this passage can be less than a day during growing seasons. This quick turnover suggests that human activities, like agriculture, are intensifying the natural water cycle.
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By measuring how fast water moves through vegetation, the study provides valuable data for predicting how events like droughts and wildfires might impact the water cycle. It presents a more detailed picture of the terrestrial water cycle, showing that plant water transit is as essential as ocean and atmospheric flow.
Understanding the speed at which water cycles through plants helps in better estimating the time a drop of water takes to complete its terrestrial journey. This knowledge is critical, particularly in a world where climate change could further alter these dynamics. The study’s findings emphasize the need to include vegetation in water cycle models for more accurate predictions and better management of water resources.
Implications on Climate
The rapid transit of water through plants has significant implications for climate patterns. As plants quickly release water back into the atmosphere, this process can influence weather phenomena and climate dynamics. Understanding this rapid turnover time helps clarify how changes in vegetation and land use could impact the global water cycle and weather patterns.
- Fast water transit in croplands can lead to more frequent heavy rain events.
- Rapid recycling of water affects regional humidity levels and cloud formation.
- Changes in vegetation impact the speed and distribution of water cycles globally.
The swift movement of water from soil through plants and back to the atmosphere can intensify the hydrological cycle. This means that rainwater could be returning to the sky faster, potentially leading to more extreme weather events, such as intense rainfall and storms. Since croplands have the fastest water transit time, extensive agriculture might be accelerating this process even further.
Changes in land use, like deforestation, could disrupt this delicate balance in the water cycle. Without trees, which typically have a longer transit time for water, regions might experience a shift in their climate. The removal of forests could mean the local recycling of water is slowed down, potentially altering precipitation patterns and increasing the risk of droughts.
Additionally, climate events like droughts or wildfires could alter water transit dynamics. These events might change how efficiently plants can recycle water. This makes plants' role in water cycles crucial and sensitive.
Understanding these mechanisms allows us to better predict and respond to climate changes. Knowledge of how water quickly moves through plants gives scientists a deeper insight into forecasting and managing weather-related impacts. By recognizing the critical role plants play, we can consider new ways to manage land and water resources to mitigate adverse climate effects. This study emphasizes the necessity to include plant dynamics in our understanding of the water cycle and climate systems.
The study is published here:
https://www.nature.com/articles/s44221-024-00365-9and its official citation - including authors and journal - is
Felton, A.J., Fisher, J.B., Hufkens, K. et al. Global estimates of the storage and transit time of water through vegetation. Nat Water, 2025 DOI: 10.1038/s44221-024-00365-9
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