THE NEW CLIMATE

When one of my best friends called to invite me on a girls' trip to Alaska in late July, I answered before she could finish the sentence. One of my childhood dreams was finally coming true.

But the biggest surprise came once we were there.

One morning, we were kayaking through a quiet fjord when something unexpected happened. Not far from our boats, a whale surfaced. The blow appeared first. Then a long dark back rolled slowly through the water before disappearing again. The entire moment lasted only a few seconds, but it is the kind of encounter that stays with you. Especially when four scientists are sitting in those kayaks. One of them happened to be a marine mammal biologist.

Moments like that are a reminder that whales are not just large animals. They are survivors of a difficult history.

For much of the twentieth century, whales were hunted at an industrial scale. Modern whaling fleets used fast ships, explosive harpoons, and factory vessels that could process whales at sea. In only a few decades, many whale populations collapsed. Blue whales were reduced to a tiny fraction of their former numbers. Other species followed the same path.

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Blue Whale, Balaenoptera musculus — By NOAA Photo Library — anim1754, Public Domain, https://commons.wikimedia.org/w/index.php?curid=17942391

By the late twentieth century, the situation began to change. International agreements limited commercial whaling, and many countries banned it. Slowly, whale populations started to recover. It has not been quick. Whales reproduce slowly. Many species have only one calf every few years. But over time scientists began to see encouraging signs. In some regions, humpback whales returned to their former feeding grounds. Gray whales increased along the Pacific coast of North America. Blue whales began to appear again in places where they had almost vanished.

For conservation scientists, these recoveries have often been presented as one of the rare good news stories in marine conservation. Protect a species from direct hunting, and populations can rebound. Nature has the ability to recover when pressure is removed.

But the ocean that whales return to today is not the same ocean they lived in decades ago.

Over the past century, the climate system has been changing. Ocean temperatures have increased. Sea ice patterns have shifted. Currents that move nutrients through the ocean are also changing. These changes affect the base of the marine food web, where microscopic organisms support everything above them.

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Map summarising known feeding grounds of Australian southern right whales. Mean adult Antarctic krill density estimates for 2010 are derived from the KRILLPODYM model. Catches from historical American and Soviet whaling and sightings from dedicated Antarctic research surveys (IWC-IDCR/SOWER, JARPA/JARPAII, and NEWREP-A surveys are used to highlight areas of high usage by southern right whales. The red boxes show the regions analysed. The two red boxes indicate the regions analysed: a mid-latitude region spanning 70°−170°E and 35°−50°S, and a high-latitude region spanning 70°−170°E and 55°−70°S — Charlton et al., 2026

To understand why this matters for whales, it helps to think about what many of them eat. Some of the largest animals that have ever lived feed on surprisingly small prey. Blue whales and humpback whales rely heavily on krill, small shrimp-like animals that gather in dense swarms. A single whale can consume several tons of krill in one day during feeding season.

Krill themselves depend on specific environmental conditions. In polar and subpolar regions, they are closely linked to sea ice and seasonal plankton blooms. When sea ice forms and melts, it helps control when and where microscopic algae grow. Those algae feed krill. The krill feed whales.

If those environmental conditions shift, the entire food chain can shift with them.

Over the past few decades, researchers studying the Southern Ocean have noticed signs that krill populations may be changing. Some regions have seen declines. Other regions show shifts in where krill concentrate. These patterns are complex and vary from place to place, but many scientists agree that climate change is likely playing a role.

This matters because whales recovering from past hunting still depend on these food resources to rebuild their populations.

A recent study in Scientific Reports adds another piece of evidence to this story. Researchers examined how climate-driven changes in ocean conditions could influence the recovery of baleen whales in the Southern Ocean. Instead of focusing only on the whales themselves, they looked closely at the environmental conditions that shape krill availability and feeding opportunities.

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Time series of calving interval (CI) and environmental indices for southern right whales off southwest Australia from 1996–2024. Solid black lines represent annual means, and vertical grey error bars indicate one standard deviation. Points are coloured based on their deviation from the long-term mean: red indicates values more than 10% above the mean, blue values more than 10% below, and white values within ± 10%. Environmental variables include the Oceanic Niño Index (ONI), Antarctic Oscillation (AAO), Antarctic sea ice concentration anomaly (SIC), cumulative summer chlorophyll-a concentration for mid and high latitudes (Chl), and mid-latitude sea surface temperature (SST) — Charlton et al., 2026

Their analysis combined ecological observations, climate records, and models of whale population recovery. The goal was not to question whether whales are recovering. In many cases they clearly are. The question was more subtle. Could changes in the ocean environment slow that recovery?

The results suggest that this is possible.

As ocean conditions change, the distribution and abundance of krill may also change. When krill become less predictable or less concentrated, whales must spend more energy searching for food. Feeding seasons may become less productive. Over time, this can affect how quickly whale populations grow.

The key point is not that whale recovery has stopped. Many populations are still increasing. But the pace of recovery may depend not only on protection from hunting, but also on how the climate system shapes the ecosystems whales rely on.

This idea is familiar to ecologists. Species rarely respond to a single factor in isolation. Removing one threat does not mean the environment automatically returns to the conditions that existed before that threat appeared. The system itself may have changed.

In marine ecosystems, these changes can be difficult to see because they happen across enormous areas and long timescales. A whale migration can cover thousands of kilometers. Ocean productivity can vary from year to year. Climate signals unfold slowly.

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Five-year composite anomalies of Antarctic sea ice concentration (SIC) and sea surface temperature (SST) from 1995 to 2024. Each panel shows spatial anomalies relative to the long-term mean (1995–2024), averaged over five-year periods. Anomalies in SIC are shown in the inner sector, corresponding to high latitude foraging grounds, using a green–purple scale. Anomalies in SST are shown in the outer sector, corresponding to mid latitude foraging grounds, using a red–blue scale. Positive SST anomalies (red) and negative SIC anomalies (green) indicate warmer-than-average and less ice-covered conditions, respectively. Map orientation was chosen to maximise use of page space — Charlton et al., 2026

But when researchers combine long records of environmental data with ecological studies, patterns begin to appear.

The emerging picture is one where conservation success and environmental change interact. Protection from hunting allows whale populations to grow. At the same time, climate change can alter the food resources that support that growth.

This does not erase the success of whale conservation. If anything, it shows how important those protections were. Without the ban on large-scale commercial whaling, many whale species might not exist today in numbers large enough to recover at all.

Instead, whales are returning to the oceans. In some regions people now see them regularly during migrations and feeding seasons. Researchers track their movements with satellite tags and acoustic monitoring. Long-term population surveys show steady increases for several species.

What the new research highlights is the next challenge. Conservation does not end when hunting stops. It continues as ecosystems themselves change.

For scientists who study marine ecosystems, whales offer a clear example of how different environmental pressures can overlap. Human activity removed millions of whales during the twentieth century. Policy decisions reduced that pressure. Now, environmental change introduces a different kind of influence.

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Mean apparent calving intervals box plot for all intervals (A), and annual proportion of identified female southern right whales (Eubalaena australis) on a three, four and five-year apparent calving interval in years, (B) at Head of Bight, South Australia (1996–2024) — Charlton et al., 2026

Understanding how these forces interact helps researchers anticipate what recovery might look like in the future. It also reminds us that conservation successes do not happen in isolation. Protecting species is only part of the picture. The ecosystems that support them must remain productive enough to sustain their return.

Watching a whale surface in the open ocean still feels like witnessing something ancient and resilient. These animals survived millions of years of natural climate shifts long before humans existed. Today, their future depends on a combination of careful protection and a changing environment that scientists are still working to understand.

The story of whale recovery is not finished. But it already shows something important. When humans reduce direct pressure on wildlife, nature often responds. The question now is how that recovery unfolds in an ocean that continues to change.

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