Friday, 2 June 2017

Tech Here's what Earth might look like in 100 years — if we're lucky

Tech Here's what Earth might look like in 100 years — if we're lucky


Even if the US remains part of the Paris climate accord, the best situation we can hope for is pretty worrisome.
U.S. President Donald Trump waves as he walks on the South Lawn of the White House in Washington play U.S. President Donald Trump waves as he walks on the South Lawn of the White House in Washington
(Thomson Reuters)
  President Donald Trump on Thursday announced his intent to withdraw the US from the Paris climate accord.
"We're getting out, but we will start to negoatiate to see if we can make a deal that is fair," Trump claimed during a televised briefing from the White House.
Trump's widely denounced decision comes on the heels of the hottest year the world has seen since 1880 — when scientists first started keeping global temperature logs — and the fifth annual heat record of the past dozen years.
Overall, planet Earth has warmed 2.3 degrees Fahrenheit (1.26 degrees Celsius) above preindustrial averages, which is dangerously close to the 2.7-degree-Fahrenheit (1.5-degree-Celsius) limit set by international policymakers for global warming. (Some argue this cutoff is arbitrary, though it could still rein in some of the most disruptive changes to human civilization.)
"There's no stopping global warming," Gavin Schmidt, a climate scientist who is the director of NASA's Goddard Institute of Space Studies, previously told Business Insider. "Everything that's happened so far is baked into the system."
That means that even if carbon emissions were to drop to zero tomorrow, we'd still be watching human-driven climate change play out for centuries. And we all know emissions aren't going to stop. So the key thing now, Schmidt said, is to slow climate change down enough to make sure we can adapt to it as painlessly as possible.
This is what the Earth could look like within 100 years if we succeed in curbing climate change with international agreements like the Paris climate accord (barring huge leaps in renewable energy or carbon-capture technology).
Sarah Kramer wrote a previous version of this post.

"I think the 1.5-degree [2.7-degree F] target is out of reach as a long-term goal," Schmidt said. He estimated that we will blow past that by about 2030.

"I think the 1.5-degree [2.7-degree F] target is out of reach as a long-term goal," Schmidt said. He estimated that we will blow past that by about 2030. play "I think the 1.5-degree [2.7-degree F] target is out of reach as a long-term goal," Schmidt said. He estimated that we will blow past that by about 2030.
(Stephane Mahe/Reuters)


But Schmidt is more optimistic about staying at or under 3.6 degrees F, or 2 degrees C, above preindustrial levels. That's the level of temperature rise the UN hopes to avoid.

But Schmidt is more optimistic about staying at or under 3.6 degrees F, or 2 degrees C, above preindustrial levels. That's the level of temperature rise the UN hopes to avoid. play But Schmidt is more optimistic about staying at or under 3.6 degrees F, or 2 degrees C, above preindustrial levels. That's the level of temperature rise the UN hopes to avoid.
(Vincent Kessler/Reuters)


Let's assume that we land somewhere between those two targets. At the end of this century, we'd be looking at a world that is on average about 3 degrees Fahrenheit above where we are now.

Let's assume that we land somewhere between those two targets. At the end of this century, we'd be looking at a world that is on average about 3 degrees Fahrenheit above where we are now. play Let's assume that we land somewhere between those two targets. At the end of this century, we'd be looking at a world that is on average about 3 degrees Fahrenheit above where we are now.
(NASA)


But average surface temperature alone doesn't paint a full picture of climate change. Temperature anomalies — or how much the temperature of a given area is deviating from what would be "normal" in that region — will swing wildly.

But average surface temperature alone doesn't paint a full picture of climate change. Temperature anomalies — or how much the temperature of a given area is deviating from what would be "normal" in that region — will swing wildly. play But average surface temperature alone doesn't paint a full picture of climate change. Temperature anomalies — or how much the temperature of a given area is deviating from what would be "normal" in that region — will swing wildly.
(Oli Scarff/Getty)
Source: Business Insider


For example, the temperature in the Arctic Circle soared above freezing for one day in 2016 — that's extraordinarily hot for the arctic. Those types of abnormalities will start happening a lot more.

For example, the temperature in the Arctic Circle soared above freezing for one day in 2016 — that's extraordinarily hot for the arctic. Those types of abnormalities will start happening a lot more. play For example, the temperature in the Arctic Circle soared above freezing for one day in 2016 — that's extraordinarily hot for the arctic. Those types of abnormalities will start happening a lot more.
(Bob Strong/Reuters)
Source: Washington Post


That means years like 2016, which had the lowest sea-ice extent on record, will become more common. Summers in Greenland could become ice-free by 2050.

That means years like 2016, which had the lowest sea-ice extent on record, will become more common. Summers in Greenland could become ice-free by 2050. play That means years like 2016, which had the lowest sea-ice extent on record, will become more common. Summers in Greenland could become ice-free by 2050.
(NASA Goddard Flickr)
Source: Journal of Advances in Modeling Earth Systems


In the summer of 2012, 97% of the Greenland Ice Sheet's surface started to melt. That's typically a once-in-a-century occurrence, but we could see extreme surface melt like that every six years by end of the century.

In the summer of 2012, 97% of the Greenland Ice Sheet's surface started to melt. That's typically a once-in-a-century occurrence, but we could see extreme surface melt like that every six years by end of the century. play In the summer of 2012, 97% of the Greenland Ice Sheet's surface started to melt. That's typically a once-in-a-century occurrence, but we could see extreme surface melt like that every six years by end of the century.
(Flickr/Ville Miettinen)
Source: Climate Central, National Snow & Ice Data Center


On the bright side, ice in Antarctica will remain relatively stable, making minimal contributions to sea-level rise.

On the bright side, ice in Antarctica will remain relatively stable, making minimal contributions to sea-level rise. play On the bright side, ice in Antarctica will remain relatively stable, making minimal contributions to sea-level rise.
(Andreas Kambanis on Flickr)
Source: Nature


However, unexpected ice shelf collapses could surprise researchers with extra sea-level rise.

A 300-foot-wide, 70-mile-long rift in Antarctica's Larsen C Ice Shelf, as seen in November 2016. play A 300-foot-wide, 70-mile-long rift in Antarctica's Larsen C Ice Shelf, as seen in November 2016.
(John Sonntag/IceBridge/NASA Goddard Space Flight Center)
Source: Business Insider


Even in our best-case scenarios, oceans are on track to rise 2 to 3 feet by 2100. That could displace up to 4 million people.

Even in our best-case scenarios, oceans are on track to rise 2 to 3 feet by 2100. That could displace up to 4 million people. play Even in our best-case scenarios, oceans are on track to rise 2 to 3 feet by 2100. That could displace up to 4 million people.
(Thomson Reuters)
Source: NASA, Time


Oceans absorb about one-third of all carbon dioxide in the atmosphere, causing them to warm and become more acidic. Rising temperatures will therefore cause oceans to acidify more around the globe.

Oceans absorb about one-third of all carbon dioxide in the atmosphere, causing them to warm and become more acidic. Rising temperatures will therefore cause oceans to acidify more around the globe. play Oceans absorb about one-third of all carbon dioxide in the atmosphere, causing them to warm and become more acidic. Rising temperatures will therefore cause oceans to acidify more around the globe.
(Brandi Mueller for Argunners Magazine)
Source: International Geosphere-Biosphere Program


In the tropics, that means nearly all coral reef habitats could be devastated. Under our best-case scenario, half of all tropical coral reefs are still threatened.

In the tropics, that means nearly all coral reef habitats could be devastated. Under our best-case scenario, half of all tropical coral reefs are still threatened. play In the tropics, that means nearly all coral reef habitats could be devastated. Under our best-case scenario, half of all tropical coral reefs are still threatened.
(Matt Kieffer/flickr)
Source: International Geosphere-Biosphere Program


And even if we curb emissions, summers in the tropics could see a 50% increase their extreme-heat days by 2050. Farther north, 10% to 20% of the days in a year will be hotter.

And even if we curb emissions, summers in the tropics could see a 50% increase their extreme-heat days by 2050. Farther north, 10% to 20% of the days in a year will be hotter. play And even if we curb emissions, summers in the tropics could see a 50% increase their extreme-heat days by 2050. Farther north, 10% to 20% of the days in a year will be hotter.
(Lionel Cironneau/AP)
Source: Environmental Research Letters


Without controlling our emissions (a business-as-usual scenario), the tropics would stay at unusually hot temperatures all summer long. In the temperate zones, 30% or more of the days would have temperatures that we currently consider unusual.

Without controlling our emissions (a business-as-usual scenario), the tropics would stay at unusually hot temperatures all summer long. In the temperate zones, 30% or more of the days would have temperatures that we currently consider unusual. play Without controlling our emissions (a business-as-usual scenario), the tropics would stay at unusually hot temperatures all summer long. In the temperate zones, 30% or more of the days would have temperatures that we currently consider unusual.
(AP Photo/Matt York)
Source: Environmental Research Letters


Even a little bit of warming will likely strain water resources. In a 2013 paper, scientists projected that the world will start to see more intense droughts more often. Left unchecked, climate change may cause severe drought across 40% of all land — double what it is today.

Even a little bit of warming will likely strain water resources. In a 2013 paper, scientists projected that the world will start to see more intense droughts more often. Left unchecked, climate change may cause severe drought across 40% of all land — double what it is today. play Even a little bit of warming will likely strain water resources. In a 2013 paper, scientists projected that the world will start to see more intense droughts more often. Left unchecked, climate change may cause severe drought across 40% of all land — double what it is today.
(Reuters)
Source: PNAS


And then there's the weather. If the extreme El Niño event of 2015-2016 was any indication, we're in for more natural disasters — storm surges, wildfires, and heat waves are on the menu for 2070 and beyond.

And then there's the weather. If the extreme El Niño event of 2015-2016 was any indication, we're in for more natural disasters — storm surges, wildfires, and heat waves are on the menu for 2070 and beyond. play And then there's the weather. If the extreme El Niño event of 2015-2016 was any indication, we're in for more natural disasters — storm surges, wildfires, and heat waves are on the menu for 2070 and beyond.
(REUTERS/Max Whittaker)
Source: Environment360


Right now, humanity is standing on a precipice. If we ignore the warning signs, we could end up with what Schmidt envisions as a "vastly different planet" — roughly as different as our current climate is from the most recent ice age.

Right now, humanity is standing on a precipice. If we ignore the warning signs, we could end up with what Schmidt envisions as a "vastly different planet" — roughly as different as our current climate is from the most recent ice age. play Right now, humanity is standing on a precipice. If we ignore the warning signs, we could end up with what Schmidt envisions as a "vastly different planet" — roughly as different as our current climate is from the most recent ice age.
(Reuters)


Or we can innovate solutions. Many of the scenarios laid out here assume we're reaching negative emissions by 2100 — that is, absorbing more than we're emitting through carbon-capture technology.

Or we can innovate solutions. Many of the scenarios laid out here assume we're reaching negative emissions by 2100 — that is, absorbing more than we're emitting through carbon-capture technology. play Or we can innovate solutions. Many of the scenarios laid out here assume we're reaching negative emissions by 2100 — that is, absorbing more than we're emitting through carbon-capture technology.
(Reuters/Aly Song)
Source: The Guardian


Schmidt says the Earth in 2100 will be somewhere between "a little bit warmer than today and a lot warmer than today." On a planet-wide scale, that difference could mean millions of lives saved, or not.

Schmidt says the Earth in 2100 will be somewhere between "a little bit warmer than today and a lot warmer than today." On a planet-wide scale, that difference could mean millions of lives saved, or not. play Schmidt says the Earth in 2100 will be somewhere between "a little bit warmer than today and a lot warmer than today." On a planet-wide scale, that difference could mean millions of lives saved, or not.
(Benoit Tessier/ Reuters)

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