1 February 2013
I spent two weeks in the Summer of 2010 at the top of the World. To be specific I was in the middle of the Greenland Ice sheet at NEEM, about 650 miles from the North Pole, and while there I witnessed the recovery of the oldest core of ice ever recovered from Greenland. NEEM stand for North Greenland Eemian ice core. That ice core has now been analysed, and it had some BIG surprises that will affect the predictions for future sea level rise and climate change in general.
There has been some good science writing over the past week about the findings, but missing from the writing so far, is the extreme difficulty and hardship that was endured by those involved to obtain this ice core. Drilling a hole one mile deep in ice at the top of the world is not an easy task, but it was information that climate scientists desperately needed. It was accomplished over three years by a superb group of engineers and young scientists. I was honored to spend a couple of weeks with them, and to be there when the drill reached rock beneath the ice.
The big surprise from the NEEM core is that the Greenland icecap survived the warmth of the last interglacial quite well. It melted back a lot, and the spot where NEEM was located was about 150 meters lower then than now. In general there was still a big icecap in the Eemian, and it was quite a bit warmer than it is now.
Greenland temperatures were around
8 degrees 3C warmer (Excuse the typo!) than the present although this past summer saw an amazing melt in Greenland unlike anything seen in the past hundred years. Sea level was MUCH higher in the Eemian, and many researchers believed this was due to the melting of ice in Greenland and in Antarctica. The NEEM core calls this into question, and it appears that the large rise in sea level may have come more from Antarctica. The West Antarctic Ice Shelf is known to be unstable, but could it be much more sensitive to rising temperatures than was thought? It seems strange when you think about, it but research grants to look at ice in Greenland may end up telling us a lot about Antarctica.
A paper announcing the findings was published in NATURE this past week, and the editor’s note is a good summary:
A detailed record of Eemian climate
The Greenland ice sheet is losing mass and contributing to ongoing sea level rise, but an incomplete understanding of its changes during the last interglacial 130,000–115,000 years ago, termed the Eemian, have hampered firm predictions. Now an international team has successfully reconstructed the Eemian climate record from the new NEEM ice core. The record shows that in spite of a climate 8 °C warmer than that of the past millennium, the thickness of the ice sheet decreased by only a few hundred metres. In addition, the ice core shows that there was significant surface melt in the north-central parts of the ice sheet during the Eemian, conditions we might soon see again, as demonstrated by melt layers formed at NEEM by the warm temperatures observed over Greenland in July 2012.
An excellent piece in nature describing more fully the impact of this ice core and why it is so important is HERE.
Below is a collection of videos I shot at NEEM, and hopefully they give you an idea what it was like to be there. Real science is not setting around in a white coat and staring at a computer screen.
Denmark was the lead research country at NEEM, and the Neils Bohr institute at the Univ. of Copenhagen has a great summary of the findings here. I was the guest of Dorthe Dahl-Jensen and Dr. Jim White of the Univ. of Colorado the lead US Scientist. I plan on writing more on NEEM soon, with some perspective on the findings from Dr. White.