Antarctic Dispatches   Part 1 2 3

Miles of Ice Collapsing Into the Sea

We went to Antarctica to understand how changes to its vast ice sheet might affect the world. Flowing lines on these maps show how the ice is moving.

LARSEN

ICE SHELVES

BRUNT

ICE SHELF

Chile

800 miles

ANTARCTIC

PENINSULA

WEDDELL

SEA

RONNE

ICE SHELF

Berkner

Island

BELLINGSHAUSEN

SEA

Scott

Mountains

Pensacola

Mountains

Ellsworth

Mountains

EAST

ANTARCTICA

WEST

ANTARCTICA

AMUNDSEN

SEA

South

Pole

AMERY

ICE SHELF

TRANSANTARCTIC

MOUNTAINS

AMUNDSEN

SEA

Where

we flew

Sulzberger

Bay

ROSS

ICE SHELF

SHACKLETON

ICE SHELF

McMurdo

Station

ROSS

SEA

250 miles

New Zealand

1,600 miles

LARSEN

ICE SHELVES

WEDDELL

SEA

ANTARCTIC

PENINSULA

RONNE

ICE SHELF

Scott

Mountains

EAST

ANTARCTICA

WEST

ANTARCTICA

AMUNDSEN

SEA

South

Pole

AMUNDSEN

SEA

Where we

flew

ROSS

ICE SHELF

ROSS

SEA

McMurdo

Station

250 miles

New Zealand

1,600 miles

EAST

ANTARCTICA

WEST

ANTARCTICA

Where we

flew

ROSS ICE

SHELF

ROSS

SEA

500 miles

Ice sheets flow downhill, seemingly in slow motion. Mountains funnel the ice into glaciers. And ice flowing from the land into the sea can form a floating ice shelf.

ANTARCTIC

PENINSULA

WEDDELL

SEA

RONNE

ICE SHELF

BELLINGSHAUSEN

SEA

EAST

ANTARCTICA

WEST

ANTARCTICA

South

Pole

AMUNDSEN

SEA

TRANSANTARCTIC

MOUNTAINS

Where

we flew

Sulzberger

Bay

ROSS

ICE SHELF

ROSS

SEA

ANTARCTIC

PENINSULA

RONNE

ICE SHELF

EAST

ANTARCTICA

WEST

ANTARCTICA

AMUNDSEN

SEA

South

Pole

Where

we flew

Sulzberger

Bay

ROSS

ICE SHELF

ROSS

SEA

WEDDELL

SEA

WEST

ANTARCTICA

Where

we flew

ROSS

ICE SHELF

ROSS

SEA

Glaciers in certain areas have been undercut by warmer ocean waters, and the flow of ice is getting faster and faster.

Pensacola

Mountains

Abbot

Ice Shelf

Jones

Mountains

Ellsworth

Mountains

Thurston

Island

Pine Island

Glacier

WEST

ANTARCTICA

AMUNDSEN

SEA

Whitmore

Mountains

Thwaites

Glacier

Kohler

Range

Getz

Ice Shelf

Pensacola

Mountains

Ellsworth

Mountains

Pine Island

Glacier

WEST

ANTARCTICA

Thwaites

Glacier

AMUNDSEN

SEA

Getz

Ice Shelf

BELLINGSHAUSEN

SEA

Pine Island

Glacier

Thwaites

Glacier

AMUNDSEN

SEA

WEST

ANTARCTICA

Executive

Committee Range

This is the first of three dispatches from a New York Times reporting trip to Antarctica.

The acceleration is making some scientists fear that Antarctica’s ice sheet may have entered the early stages of an unstoppable disintegration.

Because the collapse of vulnerable parts of the ice sheet could raise the sea level dramatically, the continued existence of the world’s great coastal cities — Miami, New York, Shanghai and many more — is tied to Antarctica’s fate.

Four New York Times journalists joined a Columbia University team in Antarctica late last year to fly across the world’s largest chunk of floating ice in an American military cargo plane loaded with the latest scientific gear.

Inside the cargo hold, an engineer with a shock of white hair directed younger scientists as they threw switches. Gravity meters jumped to life. Radar pulses and laser beams fired toward the ice below.

On computer screens inside the plane, in ghostly traces of data, the broad white surface of the Ross Ice Shelf began to yield the secrets hiding beneath.

“We are 9,000 miles from New York,” said the white-haired engineer, Nicholas Frearson of Columbia. “But we are connected by the ocean.”

frearson3.jpg
Nicholas Frearson, at left, in the cargo hold of an LC-130 Hercules.

A rapid disintegration of Antarctica might, in the worst case, cause the sea to rise so fast that tens of millions of coastal refugees would have to flee inland, potentially straining societies to the breaking point. Climate scientists used to regard that scenario as fit only for Hollywood disaster scripts. But these days, they cannot rule it out with any great confidence.

Yet as they try to determine how serious the situation is, the scientists confront a frustrating lack of information.

Recent computer forecasts suggest that if greenhouse gas emissions continue at a high level, parts of Antarctica could break up rapidly, causing the ocean to rise six feet or more by the end of this century. That is double the maximum increase that an international climate panel projected only four years ago.

But those computer forecasts were described as crude even by the researchers who created them. “We could be decades too fast, or decades too slow,” said one of them, Robert M. DeConto of the University of Massachusetts, Amherst. “There are still some really big question marks about the trajectory of future climate around Antarctica.”

Alarmed by the warning signs that parts of the West Antarctic ice sheet are becoming unstable, American and British scientific agencies are joining forces to get better measurements in the main trouble spots. The effort could cost more than $25 million and might not produce clearer answers about the fate of the ice until the early 2020s.

For scientists working in Antarctica, the situation has become a race against time.

Even as the threat from global warming comes into sharper focus, these scientists understand that political leaders — and cities already feeling the effects of a rising sea — need clearer forecasts about the consequences of emissions. That urgent need for insight has led scientists from Columbia to spend the past two Antarctic summers flying over the Ross Ice Shelf, a floating chunk of ice larger than California.

The Ross shelf helps to slow the flow of land ice from Antarctica into the ocean. Compared with other parts of Antarctica, the shelf seems stable now, but computer forecasts suggest that it might be vulnerable to rapid collapse in the next few decades.

The project to map the structure and depth of the ice shelf in detail, funded by American taxpayers through the National Science Foundation, puts Columbia and its partner institutions on the front lines of one of the world’s most urgent scientific and political problems.

“Our goal is to understand how to predict what’s going to happen to the ice sheets,” said Robin E. Bell, the lead Columbia scientist in charge of the effort. “We really don’t know right now.”

Remote as Antarctica may seem, every person in the world who gets into a car, eats a steak or boards an airplane is contributing to the emissions that put the frozen continent at risk. If those emissions continue unchecked and the world is allowed to heat up enough, scientists have no doubt that large parts of Antarctica will melt into the sea.

But they do not know exactly what the trigger temperature might be, or whether the recent acceleration of the ice means that Earth has already reached it. The question confronting society, said Richard B. Alley, a climate scientist at Pennsylvania State University, is easier to ask than to answer:

“How hot is too hot?”

In the immersive video below, a military cargo plane flies over the edge of the Ross Ice Shelf. The orange and gray pod beneath the window will map the structure of the shelf with radar, a laser and other sensors.

Continue to Part 2

Looming Floods, Threatened Cities

Antarctic Dispatches is a three-part series from the seventh continent. Written by Justin Gillis. Maps and graphics by Derek Watkins and Jeremy White. Photographs by Jonathan Corum. Video by Evan Grothjan and Graham Roberts. Additional production by Gregor Aisch, Larry Buchanan and Rumsey Taylor. Experience what it’s like above and below the Antarctic ice in virtual reality, or read the story behind our reporting trip.

Map sources: Lamont-Doherty Earth Observatory of Columbia University; British Antarctic Survey; NASA Earth Observatory; Natural Earth; Bright Earth e-Atlas Basemap