29/03/2018

'Harder And Riskier': Carbon Removal Needed If Paris Goals Don't Rise

Fairfax - Peter Hannam

Greenhouse gas emission cuts must be at least 20 per cent deeper than pledged under the Paris climate accord or the world will have to begin the costly direct removal of atmospheric carbon to avoid dangerous climate change, a new study argues.
The Germany-based researchers examined the action needed if nations failed to deliver greater carbon curbs by 2030 but still kept global warming to under 2 degrees, compared with pre-industrial levels.
"Each tonne of CO2 we don't emit, we don't have to remove from the atmosphere afterwards in an expensive and strenuous way," said Jessica Strefler from the Potsdam Institute for Climate Impact Research and the lead author of the paper published on Thursday in Environmental Research Letters.
Emissions impossible? Delays in cutting emissions make it more likely that carbon will have to be directly captured if dangerous climate change is to be avoided.
Computer simulations indicate an industry "comparable" to the size of the global petroleum sector, and able to capture and store at least 5 billion tonnes of C02 annually, will be required - and possibly much larger.
Such carbon removal - whether by reafforestation ($31 per tonne) or direct air capture ($652 per tonne) - would be costly.  "One way of paying for these technologies is imposing a price on carbon emissions and using these revenues to pay for carbon dioxide removal," Dr Strefler told Fairfax Media.
Strengthened Paris goals - known as nationally determined contributions (NDCs) - could preclude the need for carbon extraction but only if they were sharply increased.
"We would have to roughly halve 2030 emissions compared to current pledges, and halve them again every decade until 2050," Dr Strefler said. "If we do not strengthen the NDCs significantly, CO2 reduction will be necessary to achieve the 2-degree target."
The projections underscore the challenges nations will face when delegates gather in Katowice, Poland, in December. Australia, which has pledged to cut 2005-level carbon emissions by 26-28 per cent by 2030, will be among the countries pressed to do more.
Evidence of climate change mounts, and includes the past four years recording "exceptionally warm" temperatures.  Last year was the hottest year on record that was not an El Nino year, while the Arctic - the world's fastest-changing region - just completed its warmest winter.

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Pep Canadell, a research scientist with the CSIRO and executive director of the Global Carbon Project, said the German study used a simplified model that, if anything, underestimated the scale of the challenge.
For instance, it assumed a global carbon price of $US50 per tonne by 2020 for a cost-effective scenario - "something very far from our real world", Dr Canadell said.
"For every year we delay reaching peak emissions and decline, the harder and riskier it will get to avoid the worst impacts of climate change," he said.
"[It's] riskier because we will need to rely more on CO2 removal at scales well beyond what we can achieve from planting trees and producing ever more bioenergy."
An inter-generational ethical issue is rapidly emerging, "leaving the hard parts" for the next generation to take care of, such as the removal of atmospheric CO2, he said.
Preliminary data for 2017 shows emissions from fossil fuels and industry rose 1.5 per cent from a year earlier, resuming growth after stabilising for the first time in decades between 2014 and 2016,  the World Meteorological Organisation said in its State of the Global Climate in 2017 report.

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10 Things: All About Ice

NASA - Kristen Walbolt

Credit: Michael Studinger, Operation IceBridge project scientist. More on this image

1. Earth’s changing cryosphere
This year, NASA will launch two satellite missions that will increase our understanding of Earth’s frozen reaches. Snow, ice sheets, glaciers, sea ice and permafrost, known as the cryosphere, act as Earth’s thermostat and deep freeze, regulating temperatures by reflecting heat from the Sun and storing most of our fresh water.

2. GRACE-FO: Building on a legacy and forging ahead
The next Earth science satellites set to launch are twins! The identical satellites of the GRACE Follow-On mission will build on the legacy of their predecessor GRACE by also tracking the ever-changing movement of water around our planet, including Earth’s frozen regions.GRACE-FO, a partnership between NASA and the German Research Center for Geosciences (GFZ), will provide critical information about how the Greenland and Antarctic ice sheets are changing. GRACE-FO, workingtogether, will measure the distance between the two satellites to within 1 micron (much less than the width of a human hair) to determine the mass below.
Greenland has been losing about 280 gigatons of ice per year on average, and Antarctica has lost almost 120 gigatons a year with indications that both melt rates are increasing. A single gigaton of water would fill about 400,000 Olympic-sized swimming pools; each gigaton represents a billion tons of water.

3. ICESat-2: 10,000 laser pulses a second
In September, NASA will launch ICESat-2, which uses a laser instrument to precisely measure the changing elevation of ice around the world, allowing scientists to see whether ice sheets and glaciers are accumulating snow and ice or getting thinner over time. ICESat-2 will also make critical measurements of the thickness of sea ice from space. Its laser instrument sends 10,000 pulses per second to the surface and will measure the photons’ return trip to satellite. The trip from ICESat-2 to Earth and back takes about 3.3 milliseconds.

4. Seeing less sea ice

Summertime sea ice in the Arctic Ocean now routinely covers about 40 percent less area than it did in the late 1970s, when continuous satellite observations began. This kind of significant change could increase the rate of warming already in progress and affect global weather patterns.

5. The snow we drink
In the western United States, 1 in 6 people rely on snowpack for water. NASA field campaigns such as the Airborne Snow Observatory and SnowEx seek to better understand how much water is held in Earth’s snow cover, and how we could ultimately measure this comprehensively from space.

6. Hidden in the ground
Permafrost – permanently frozen ground in the Arctic that contains stores of heat-trapping gases such as methane and carbon dioxide – is thawing at faster rates than previously observed. Recent studies suggest that within three to four decades, this thawing could be releasing enough greenhouse gases to make Arctic permafrost a net source of carbon dioxide rather than a sink. Through airborne and field research on missions such as CARVE and ABoVE – the latter of which will put scientists back in the field in Alaska and Canada this summer – NASA scientists are trying to improve measurements of this trend in order to better predict global impact.

7. Breaking records over cracking ice
Last year was a record-breaking one for Operation IceBridge, NASA’s aerial survey of polar ice. For the first time in its nine-year history, the mission carried out seven field campaigns in the Arctic and Antarctic in a single year. In total, the IceBridge scientists and instruments flew over 214,000 miles, the equivalent of orbiting the Earth 8.6 times at the equator.
On March 22, NASA completed the first IceBridge flight of its spring Arctic campaign with a survey of sea ice north of Greenland. This year marks the 10th Arctic spring campaign for IceBridge. The flights continue until April 27 extending the mission’s decade-long mapping of the fastest-changing areas of the Greenland Ice Sheet and measuring sea ice thickness across the western Arctic basin.

8. OMG
Researchers were back in the field this month in Greenland with NASA’s Oceans Melting Greenland survey. The airborne and ship-based mission studies the ocean’s role in melting Greenland’s ice. Researchers examinetemperatures, salinity and other properties of North Atlantic waters along the more than 27,000 miles (44,000 km) of jagged coastline.

9. DIY glacier modeling
Computer models are critical tools for understanding the future of a changing planet, including melting ice andrising seas. A new NASA sea level simulator lets you bury Alaska’s Columbia glacier in snow, and, year by year, watch how it responds. Or you can melt the Greenland and Antarctic ice sheets and trace rising seas as they inundate the Florida coast.

10. Ice beyond Earth
Ice is common in our solar system. From ice packed into comets that cruise the solar system to polar ice caps on Mars to Europa and Enceladus—the icy ocean moons of Jupiter and Saturn—water ice is a crucial ingredient in the search for life was we know it beyond Earth.

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