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越境企画
How Do We Restore the Land We Once Burned?
For generations, Ireland’s peatlands provided fuel, jobs, and warmth. Today, the country is bringing water back to drained bogs. Explore how peatland restoration is reshaping carbon conservation, local livelihoods, and the meaning of a just transition. -
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When Glaciers Retreat, How Does a Country’s Landscape Change?
Beyond Iceland’s glacial lagoons lies a changing relationship between ice, water, electricity, and livelihoods. As glaciers retreat, they reshape the landscape—and the choices facing the people who depend on it. -
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As the Drift Ice Retreats, What Changes in Shiretoko’s Sea?
Hokkaido’s drift ice is more than a winter spectacle. Its formation, movement, and melting help shape the seasonal rhythms of Shiretoko’s sea. What might change as the ice retreats? -
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The Fish Arriving at the Harbor Have Changed
The fish arriving at a harbor carry clues to a changing sea. Explore how landing records and fishers’ observations help reveal shifts in marine ecosystems—and how coastal communities can adapt their fisheries, businesses, and food traditions. -
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What Is Happening Beneath Seas Where Fish Have Disappeared?
The sea may look unchanged while oxygen levels fall beneath its surface. Explore how ocean warming and excessive nutrient inputs can affect the places where fish and other marine organisms live—and why changes in catches require more than one explanation. -
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Why Do Peatlands Burn for Palm Oil? Indonesia’s Wetlands and the Hidden Costs of Global Consumption
Everyday products connect consumers to Indonesia’s peatlands through palm oil supply chains. Behind low prices lie the costs of drainage, fires and carbon emissions—and the challenge of protecting wetlands while supporting farmers. -
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Why Peatlands Keep Burning Underground: Wetland Fires and Carbon Stored for Millennia
Peat fires can smoulder beneath the surface long after visible flames disappear. The deeper cause often begins years earlier, when drainage turns wet, carbon-rich soil into fuel. -
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When the Ice Disappears, the Mountain Begins to Move: Permafrost Thaw and the Risk of Rockfall
Retreating glaciers expose rock slopes to new conditions, while warming permafrost can weaken ice within their fractures. What do these changes mean for mountain communities and infrastructure? -
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After the Water Rises, the River Runs Thin: Peak Water and the Future of Glacier-Fed Rivers
As glaciers melt, rivers may carry more water for a time. Peak water marks the point when that contribution begins to fall, creating new challenges for farms, cities, hydropower and ecosystems. -
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How Distant Smoke Melts Himalayan Glaciers: Black Carbon on the Snow
Smoke from distant cities and fires can reach Himalayan glaciers. The black carbon it carries darkens snow, increases heat absorption and adds pressure to the water sources that sustain communities downstream. -
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What Flows Out When Glaciers Melt? The Risk of Pollution Preserved in Ice
Glaciers preserve traces of past pollution alongside records of Earth’s climate. As the ice melts, PFAS, metals and other substances may move into rivers and lakes, raising new questions for downstream communities. -
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Where Did the Water Meant for Lake Urmia Go?
Lake Urmia’s retreat has exposed vast salt flats in northwestern Iran. Its decline reflects both a changing climate and decisions about how water is used for farming across the watershed. -
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Has Lake Chad Really Disappeared?
Lake Chad shrank dramatically in the past, but its story is not one of steady disappearance. Its changing shoreline reshapes farmland, fishing grounds, pasture, and daily life across four countries. -
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The Lake in the Sky Is Quietly Shrinking: Falling Water Levels and Pollution Threaten Lake Titicaca
Lake Titicaca connects the lives and ecosystems of Peru and Bolivia. As water levels fall and pollution persists, its changing shores threaten totora wetlands, native species, and the communities that depend on the lake. -
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When a Lake Disappears, Its Bed Takes to the Sky: How the Shrinking Great Salt Lake Is Changing Ecosystems and Air
As the Great Salt Lake shrinks, its exposed bed changes more than the shoreline. Rising salinity threatens a vital food web, while windblown dust may carry lakebed sediments toward nearby communities. -
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When a Lake Stops Mixing: Climate Change and Lake Biwa’s “Deep Breath”
Each winter, Lake Biwa’s waters mix and carry oxygen to the lakebed. Warmer winters could weaken this “deep breath,” changing life beneath its calm surface. -
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Why Cities Built to Drain Rain Quickly Become Vulnerable to Flooding: How Pavement and Drainage Create Pluvial Flood Risk
Cities have been designed to remove rainwater as quickly as possible. But pavement and rapid drainage concentrate runoff within a shorter period, increasing pluvial flood risk. Future cities must combine drainage with storage, infiltration, and delay. -
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Do Disasters Come Only from the Sky? How “Extreme Weather” Obscures Changes in the Land
Extreme weather is intensifying, but rainfall alone does not determine the scale of a disaster. Land use, urban development, river engineering, sediment loss, exposure, and social vulnerability all shape what happens after the rain reaches the ground. -
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Can Cold Water Become Infrastructure? Protecting Rivers Through Riparian Forests, Springs, and Dam Operations
As climate change raises river temperatures, cold-water refuges are becoming essential infrastructure. Riparian forests, springs, tributaries, deep pools, fish passages, and dam operations can form a connected network that helps freshwater species survive extreme heat. -
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Rivers Have Heatwaves Too: Rising Water Temperatures Are Erasing Cold-Water Ecosystems
Climate change, drought, dams, water withdrawals, and the loss of riparian forests are warming rivers. As cold-water habitats shrink, fish need connected thermal refuges where they can escape extreme heat, survive, and reproduce. -
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Cooling Our Rooms While Warming the Planet: The Invisible Problem of HFC Refrigerants
Air conditioning protects people from dangerous heat, but many systems contain HFC refrigerants with global warming effects hundreds or thousands of times greater than carbon dioxide. How can society provide essential cooling without intensifying climate change?
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