Aivo Liiv
Alexander Orlov
Terje Aunevik
Peeter Mänd
Florian Schulz
Rene Mitt
Herve Le Goff
Andres Kaju
Tiit Pappel
Andres Rannamets
Taavi Tänav
Anti Joonas
Art Howard
Mike Dunn
Therese T Stenvall
Timo Vihma
Matti Leparanta
Torgeir Mørk
Lisa Kincaid
Lasse Stener Hansen
Raul Soome
Kristian Svarstad
Mikhail Malakhov
Assar Jõepera
Richart Sunström
Sini Häiväläinen
Carl Oskar E. Ström
Jarek Jõepera
Ulli Neumann
Ülo Tulik
Øyvind Snibsøer
Katrin Savomägi
Klaus Ryberg
Raul Lutsar
Minney Sigurðardóttir
Mart Varvas
Erik Saarts
Hillar Irves
Jaak Jaagus
Jan Karl Tholfsen
Einar Eliassen
Mart Reimann
Marko Kalve
Rain Lond
Paal Aardal Larsen
Rain Jaaksoo
Tarvo Kiudma
Reimo Olev
Argo Olesk
Rafael S.
Christoph Schimpfössl
Tarmo Mere
Margarita Tertitskaya
Kari Schrøder Hansen
Erko Jakobson
Ahti Reinup
Jukka Ikonen
Tuuli Ermel
Robin Busa
Silja Suija
Aivo Udras
Reetta Helkala
Andres Hiiemäe
Rudi Malmo
Silje Helen Christensen
Otto Riisenberg
Võru vald
M/S Stockholm
M/S Origo
ETV Osoon team
Longyearbyen Havn
S/Y Arctica II
S/Y Noorderlicht
taraexpeditions.org
Katre Palo
Taavi Palo
Kadri Palo-Juhkam
Margus Juhkam
Timo's sons
Maire Palo
Agu Palo
and Fridtjof Nansen
THE JOURNEY HAS COME TO AN END!
WE MADE IT!
AFTER 72 DAYS AND AROUND 1600 KILOMETERS WE ARE BACK AT HOME! LANDED ON THE 3rd OF JULY 2012 IN LONGYEARBYEN
On 14th March 1895, two explorers Fridtjof Nansen and Hjalmar Johansen left their icebound ship Fram and set out on skies for the North Pole. They didn’t make it to the pole, but their journey became one of the most epics, what polar history has ever seen. After latitude 86°14′ North they abandoned the attempt and retreat southwards, eventually reaching Franz Josef Land. Yet, the one of the initial plans was to reach land north of Svalbard, somewhere to the Seven Islands (Sjuøyane). This would have become better choice if these two would have make it to the pole.
“But let’s say, return trip takes 50 days. If everything has gone well, we set the course to Seven Islands, north of Spitsbergen...”
Fridtjof Nansen
Two friends, Audun Tholfsen and Timo Palo, now have a dream to take this scenario number two - if...these two brave men would have tried to return back to the Spitsbergen.
After being air dropped at the geographical North Pole, we will face to south and have to get back home. Like Nansen and his so called “burning bridges” strategy would have said: there is no way back, but only forward (Fram)!
We hope to make it to the first land within 50 days. On the land of Nordaustlandet (northeast island of the archipelago) we have placed out depot, after what we will continue towards the south until to Longyearbyen (the biggest settlement in Svalbard). We prepare for about 1400 kilometers before seeing home, but ice drift and weather can unpredictably change it.
ROUTE MAP
_Click on the map to get full-sized preview of the route!
NB! This is preliminary planned route. The real one will be posted soon in more detail.
base map source: CIA - Central Intelligence Agency
SATELLITE IMAGE OF THE ARCTIC OCEAN
_Aqua MODIS image from the Arctic Ocean in late June 2010. This is the
time we should get on land. Pay attention to the sea ice pattern and
fragments to get an idea what we might face up to! Click on image to get full-sized!
MODIS image from NASA's Earth Observatory page
UPDATED SEA ICE MAPS OF ARCTIC OCEAN
8. August 2012
_
As we are very much dependent of the sea ice conditions, then we keep now our fingers crossed for the best in spring!
You
could notice, that most of the times North coast of Spitsbergen, where
is our landing zone, is ice free. This ice free zone is caused by the
West Spitsbergen Current, what drives warm Atlantic water along the West
coast northward.
The expedition will carry out some scientific observations during on their way south across the ice. In-situ measurements are sparse in the Arctic Ocean and therefore valuable in many aspects. We will take a light set of instruments with us. Daily observations will include snow pits, snow and ice thickness measurements. Small temperature recording device called i-buttons will be mounted on the way to record temperature profile in snow pack and in the surface layer of the air. GPS measurements will help us to capture drift of the local ice floes. Regular meteorological and visual observations will be done. We will estimate for instance sea ice concentration, age and type, but also cloud cover.
