Have arrived at Zackenberg station after a spectacular trip, with the weather perfect for the trip from Constable Point, our first stop in E. Greenland, and here. I have the option of either writing a longer entry here or sending a photo, as there is no direct internet access and our satellite connection only allows us emails of a small size. For today, I’ll leave the text in favour of a picture or two. More tomorrow.

I’m writing this in Akureyri, northern Iceland, where I have to spend tonight, the departure point for the scientific charter plane to Greenland tomorrow morning. It took me 12 hours to get here, via the capital, Reykjavik. Iceland is looking very green at the moment.

This is certainly one of the world’s more picturesque little airports.

The Akureyri runway
This is not a big place, but it’s the most populated of Iceland’s towns outside the capital. It’s at the centre of North Iceland and a base for visiting a lot of this country’s natural attractions, geysers, hot pools etc, also a hub for getting to the eastern side of Greenland.

We’ve come west as well as north, and there’s two hours time difference to Germany. Of course the sun is still shining and I hope the curtains in my room are thick enough to convince me it is actually night and time for sleep. It’s a good 15 degrees cooler than home, so a good preparation for heading up to Arctic Greenland tomorrow. I met two Finnish insect scientists on the way here, also on their first trip to Zackenberg Station. They’re hoping their equipment will be waiting for them at the airport, having been sent well ahead.

Our plane will be a Twin Otter, the tried and trusty vehicle for this kind of expedition, it seems. We’ll be stopping once or twice on the way, depending on weather conditions and other scientists and supplies needing to be picked up.

More from Zackenberg tomorrow.

Greenland is the world’s largest island, with an area of some 2.2 million square km. Only around 410,000 square km of this are NOT covered by ice.
The northernmost land area in the world, situated less than 730km from the North Pole, is on Greenland, Cape Morris Jesup. The island’s southernmost point, Cape Farewell is 2,670 km south of this, so it really is a huge area, and very sparsely populated.
The island’s climate is Arctic, apart from a few sheltered valleys in South Greenland. The average temperature during the warmest month of the year does not rise above 10C.
My first destination will be Zackenberg Ecological Monitoring Station

I’ve been following the weather online, using data from Daneborg, which is around 25km from Zackenberg, and also has a base used by the station’s visiting scientists, and, incidentally, the Sirius dogsled patrol during the winter.
Weather forecasts for Daneborg

I’ll be arriving at Zackenberg, all being well, on Tuesday some time, after leaving Germany on Monday and spending a night on Iceland. More about the travel details later.
The Tuesday forecast looks good, sunshine, with a cool 4 degrees, dropping to 2 at night, although at this time of year there is not a great deal of difference, as it stays light most of the time. I’m hoping the forecast will be right and we’ll get some of that beautiful clear,blue Arctic weather. There’s always a danger of the other sort, with lots of fog.
Greenland is part of Denmark, but enjoys Home Rule, which means it deals with most of its own domestic affairs. It still has very close ties with Denmark and benefits from annual subsidies from Copenhagen, as well as free education, hospital and other services for Greenlandic citizens. The island is otherwise dependent on fishing at the moment.
The changes in the Arctic climate, which could open up access to natural resources now well under ice, will have major implications for the people of Greenland. Managing this and the whole adaptation process will be quite a challenge for the Home Rule authorities. But more about all that in the weeks to come.
More Information on Greenland from Greenland Home Rule

According to information published by the Arctic Council earlier this year summarizing a study on Snow, Water, Ice and Permaforst in the Arctic, if the ice sheet were to melt, the global seal level rise would be almost 7 meters. This figure would have devastating effects around the planet. No-one is saying this is going to happen soon, but the Greenland Ice Sheet is losing mass, and will be highly susceptible to the predicted strong warming of this part of the Arctic. I’ll be talking to the scientists working on all the complex processes which are part of climate change first-hand and finding out about their work in the field over the next few weeks.

Greenland is a key area in the global climate process. The Greenland Ice Sheet is the largest body of freshwater ice in the northern hemisphere. In recent years it has become very clear that global warming is causing the ice sheet to lose mass. Increased melting and ice discharge would have major consequences for global sea level. The warming climate is also already having a considerable impact on the lifestyle of the people of Greenland.
During the next few weeks the Ice Blog will be written from an expedition to Greenland, beginning with a visit to Zackenberg Research Station in remote North Eastern Greenland. Zackenberg is an ecosystem research and monitoring facility at 74°30’N/21°W. The station is owned by the Greenland Home Rule and is operated by the National Environmental Research Institute.
The Ice Blogger will also be visiting the interior ice sheet and the coastal glaciers, finding out first hand about the work of scientists monitoring climate change and its effects, the latest research results, and the implications both for the people of Greenland and for the rest of the world.
Deutsche Welle’s Ice Blog is part of an international broadcasting collaboration to mark the International Polar Year, partly founded by the National Science Foundation. I am extremely grateful to the NSF, Moira Rankine of Soundprint Media Inc. USA who coordinates the international project and my own organisation Deutsche Welle for making all this possible.

I’m back! And as is so often the case, there’s a lot waiting to be done that didn’t disappear while I was on holiday. So for today,I’d like to draw your attention to some people who have been looking after the icy regions of the planet while the ice-blogger was still on holiday.
IUCN and WWF jointly produce a podcast called Wild Talk.
In the latest edition, one of the topics is the 50th anniversary of the Antarctic Treaty. There’s an interview with Carl Gustav Lundin
head of the IUCN Global Marine Programme about the Treaty and the state of the Antarctic today. Worth a listen.
Ministers from the Arctic Council and the Antarctic Treaty states held their first ever joint meeting in Washington on April 6 celebrating the 50th Anniversary of the signing of the Antarctic Treaty. WWF provided the ministers with recent evidence from both the north and south poles that clearly demonstrates global temperature increases must be kept well under two degrees Celsius.
“A global average temperature rise of 2 degrees is clearly too much for the poles,” says Rob Nicoll, Manager of WWF’s Antarctic and Southern Oceans Initiative. “Scientists are already unpleasantly surprised at how quickly the impacts of warming such as sea ice loss are showing up in the polar regions, exceeding recent predictions.”
Global average warming due to climate change since the late 1800s is showing severe impacts at less than one degree, as the Arctic is warming at about twice the global average and parts of the Antarctic are also outstripping the global average. The polar regions themselves have profound and not yet fully understood impacts on climate globally, and there are fears that polar tipping points could trigger abrupt change around the world.
A forthcoming report on Antarctic Climate Change and the Environment from the Scientific Committee on Antarctic Research is expected to up previous estimates on Antarctica’s expected substantial contributions to sea level rises. Marine food chains of global significance are also under threat from warming in the Antarctic.