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Seasonal water stress in a hyperhumid forest: evidence from multiple tree-ring variables and dekadal climate analysis

Despite receiving over 4000 mm of annual rainfall, a Japanese cedar forest in Yanase, Japan, exhibits seasonal water stress during the previous July that significantly influences tree growth, as evidenced by correlations between modeled soil water and multiple tree-ring variables.

Original authors: Hitoshi Yonenobu, Koh Yasue, Yasuharu Hoshino, Motonari Ohyama, Genki Katata

Published 2026-10-23
📖 5 min read🧠 Deep dive

Original authors: Hitoshi Yonenobu, Koh Yasue, Yasuharu Hoshino, Motonari Ohyama, Genki Katata

Original paper licensed under CC BY 4.0 (https://creativecommons.org/licenses/by/4.0/). ✨ This is an AI-generated explanation of the paper below. It is not written or endorsed by the authors. For technical accuracy, refer to the original paper. Read full disclaimer

In the quiet study of how forests grow, scientists often look to the rings inside a tree trunk as a historical record. Each ring is a snapshot of a single year, capturing the weather conditions that allowed the tree to expand its girth. For decades, a simple rule of thumb has guided this field: trees in dry places grow more when it rains, while trees in cold places grow more when it is warm. But nature rarely follows such simple rules, especially in places where the rain never seems to stop. In the world's wettest forests, where thousands of millimeters of rain fall every year, the assumption has been that water is never a limiting factor. If the sky is always full of clouds and the ground is always damp, why would a tree ever struggle to find the moisture it needs to grow? This question sits at the heart of a new investigation into a specific forest in Japan, challenging the idea that abundant rainfall guarantees abundant growth.

The researchers focused on a natural forest of Japanese cedar trees in the Yanase district of Shikoku, a region known for its extreme wetness. Here, the annual rainfall exceeds 4,000 millimeters, a volume so great that it defines the area as hyperhumid. Despite this deluge, the team suspected that the trees might still face periods of thirst. The logic is that water does not simply sit on the ground; it moves. It drains away, it evaporates into the air, and the air itself can become so dry that it pulls moisture out of the leaves faster than the roots can replace it. To test this, the scientists examined 18 specific trees that had been cut down and preserved decades ago. They did not just look at the width of the rings, which shows how much the tree grew in a year. They also measured the density of the wood and separated the rings into two distinct parts: the earlywood, which forms in the spring, and the latewood, which forms later in the season. By breaking the rings down this way, they could see if different parts of the year held different clues about the tree's health.

To understand what these rings were saying, the team needed a very precise map of the weather. They combined records from local weather stations with advanced computer models of the atmosphere and land surface. They looked at temperature, rainfall, and a measure of how thirsty the air was. They also looked at the soil, using a model to estimate how much water was actually available to the tree roots in the weeks and months leading up to the growth season. The key to their discovery was looking at time in small chunks. Instead of just averaging the weather for an entire month, they examined ten-day periods. This allowed them to pinpoint exactly when the weather mattered most. They found that the trees were not reacting to the rain of the current year, but to the conditions of the summer before. Specifically, the amount of water stored in the soil during the third ten-day period of July in the previous year was the strongest predictor of how wide the tree rings would be the following spring.

This finding was surprising because July is in the middle of the rainy season in this part of Japan. Yet, the data showed a clear link: when the soil was wetter in that specific window of the previous summer, the trees grew wider the next year. When the soil was drier, the rings were narrower. This suggests that even in a forest that receives more than 4,000 millimeters of rain annually, the trees can still experience seasonal water stress. The water might be there in the clouds, but if it drains away too quickly or if the air is too dry, the tree cannot access it when it needs it most to start its spring growth. The study also found that the relationship between the weather and the tree's growth was not fixed. Over the decades, the strength of these connections changed. Sometimes the temperature of the winter months mattered more; other times, the water availability was the dominant factor. This shifting relationship indicates that the trees are not stuck in a single mode of survival but are constantly adjusting to a changing climate.

The researchers were careful to note that their findings are specific to this forest and these trees. They did not claim that every tree in a wet forest reacts this way, nor did they prove exactly how the tree physically moves water from the soil to its leaves. What they did prove is that the old assumption—that wet forests never face water stress—is incomplete. The evidence from the rings, supported by the detailed weather data, shows that the trees are sensitive to the moisture levels of the previous summer. This sensitivity persists even when the total rainfall is enormous. The study also highlighted that the trees' response to the weather is complex and changes over time. A model that works for one decade might not work for the next, suggesting that the forest's relationship with its climate is dynamic. By looking at the wood in such fine detail, the scientists have uncovered a hidden layer of struggle in a place that appears to be a paradise of water. The trees are not just growing in the rain; they are navigating a delicate balance of supply and demand, a balance that can tip even in the wettest places on Earth.

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