Category Archives: Polar Exploration

The Ice Shelf of Petermann Gletscher and its Ocean Below: Descriptions

“In 1921 owing to starvation I had to go directly from Cape Heiberg-Juergensen to our cache at Cape Agassiz … during this journey the greater part of the glacier was mapped.” –Lauge Koch, 1928

Petermann Fjord connects Petermann Gletscher to Nares Strait which in turn is connected to the Arctic Ocean in north and the Atlantic Ocean in the south (Figure-2). The track of Petermann ice island PII-2010A emphasizes this connection as the 60 meter thick section of the ice island reaches the Labrador Sea in the south within a year after its calving in 2010.

TOS2016-Fig2

PII-2010 left Petermann Fjord on the 9th of September in 2010 when it broke into segments A and B while pivoting around a real island. It flushed out of Nares Strait 10 days later when an ice-tracking beacon was placed to track the ice island. The ~60 m thick segment PII-2010A moved southward with the Baffin Island Current (Münchow et al., 2015) at an average speed of ~ 0.11 m/s past Davis Strait. Remaining on the continental shelf of the Labrador Sea, it passed Boas’ Cumberland Sound, Labrador, and reached Newfoundland in August 2011 when it melted away in a coastal cove about 3000 km from Petermann Fjord (Figure-2).

TOS2016-Fig7

Petermann Gletscher drains about 4% of the Greenland ice sheet via a network of channels and streams that extend about 750 km landward from the grounding line (Bamber et al., 2013). The glacier goes afloat at the grounding zone where bedrock, till, and ice meet the ocean waters about 600 meter below sea level (Rignot, 1996).

TOS2016-Fig3

Figure-3 shows a section of surface elevation from a laser altimeter flown on a repeat path along the glacier in April 2013 and May 2014 as part of NASA’s Operation IceBridge. Assuming hydrostatic balance, we also show basal topography below the sea surface that varies from 200 meters at the terminus to 600 meters at the grounding zone near distance zero (Figure-3). The 2013 profile has been shifted seaward by 1.25 km to match the terminus position. Note the close correspondence of large and small crevasses in 2013 and 2014 near 20, 40, and 45 km from the grounding zone.

The seaward shift of the 2013 relative to the 2014 profile implies a uniform glacier speed of about 1180 meters per year. This value is almost identical to the 1170 meters per year that we measure between 20th August of 2015 and 11th February of 2016 with a single-frequency GPS placed about 13 km seaward of the grounding zone as part of the ocean weather observatory.

We compare 2013/14 and 2015/16 velocity estimates in Figure-3 with those obtained from RadarSat interferometry between 2000 and 2008 (Joughin et al., 2010) of which I here only show three:

Figure-3 shows that glacier speeds before 2010 are stable at about 1050 m/y, but increased by about 11% after the 2010 and 2012 calving events. This increase is similar to the size of seasonal variations of glacier motions. Each summer Petermann Gletscher speeds up, because surface meltwater percolates to the bedrock, increases lubrication, and thus reduces vertical friction (Nick et al., 2012). Figure 3 presents summer velocity estimates for August of 2015 from three dual-frequency GPS. The along-glacier velocity profiles measured by these geodetic sensors in the summer follow the shape of the 2000 to 2008 winter record, however, its speeds are about 10% larger and reach 1250 m/y near the grounding zone (Figure 3).

Uncertainty in velocity of these GPS systems is about 1 m/y which we estimate from two bed rock reference stations 82 km apart. Our ice shelf observations are referenced to one of these two semi-permanent geodetic stations. Its location at Kap Schoubye is shown in Figure-1. Data were processed using the GAMIT/TRACK software distributed by MIT following methodology outlined by King (2004) to archive vertical accuracy of 2-3 centimeters which, we show next, is small relative to tidal displacements that reach 2 meters in the vertical.

TOS2016-Fig4

Figure-4 shows the entire 13 day long record of vertical glacier displacement from 30 seconds GPS measurements in August of 2015. The observed range of vertical glacier displacements diminishes from almost 2 meters about 26 km seaward of the grounding zone (GZ+26) via 0.6 meters in the grounding zone (GZ-00) to nil 20 km landward of the grounding zone (GZ-20). Anomalies of horizontal displacement are largest at GZ-00 with a range of 0.2 m (not shown) in phase with vertical oscillations (Figure-4).

More specifically, at GZ+26 we find the ice shelf to move up and down almost 2 meters roughly twice each day. This is the dominant semi-diurnal M2 tide which has a period of 12.42 hours. Notice that for each day there is also a diurnal inequality in this oscillation, that is, the two maximal (minimal) elevations oscillate from a higher to a lower High (Low) water. This is the diurnal K1 tide which has a period of 23.93 hours. And finally, all amplitudes appear modulated by some longer period that appears close to the record length of almost two weeks. This is the spring-neap cycle that is caused by a second semi-diurnal S2 tide that has a period of 12.00 hours. A formal harmonic analysis to estimate the amplitude and phases of sinusoidal oscillations at M2, K1, S2 and many more tidal constituents will be published elsewhere for both Petermann Fjord and Nares Strait. Preliminary results (not shown) reveal that the amplitudes and phases of the tidal signals at GZ+26 are identical to those observed off Ellesmere Island at 81.7 N latitude in both the 19th (Greely, 1888) and 21st century.

Hourly tidal observations at Discovery Harbor taken for 15 days by Greely in 1881 and Peary in 1909.

Hourly tidal observations at Discovery Harbor taken for 15 days by Greely in 1881 and Peary in 1909.

In summary, both historical and modern observations reveal real change in the extent of the ice shelf that moves at tidal, seasonal, and interannual time scales in response to both local and remote forcing at these times scales. Future studies will more comprehensively quantify both the time rate of change and its forcing via formal time series analyses.

P.S.: This is the second in a series of four essays that I am currently developing into a peer-reviewed submission to the Oceanography Magazine of the Oceanography Society. The work is funded by NASA and NSF with grants to the University of Delaware.

References:

Bamber, J.L., M.J. Siegert, J.A. Griggs, S. J. Marshall, and G. Spada. 2013. Palefluvial mega-canyon beneath the central Greenland ice sheet. Science 341: 997-999.

Greely, A.W. 1888. Report on the Proceedings of the United States Expedition to Lady Franklin Bay, Grinnell Land. Government Printing Office, Washington, DC.

Joughin, I., B.E. Smith, I.M. Howat, T. Scambos, and T. Moon. 2010. Greenland flow variability from ice-sheet wide velocity mapping. Journal of Glaciology 56 (197): 415-430.

King, B. 2004. Rigorous GPS data-processing strategies for glaciological applications. Journal of Glaciology 50 (171): 601–607.

Münchow, A., K.K. Falkner, and H. Melling. 2015. Baffin Island and West Greenland current systems in northern Baffin Bay. Progress in Oceanography 132: 305-317.

Nick, F.M., A. Luckman, A. Vieli, C.J. Van Der Veen, D. Van As, R.S.W. Van De Wal, F. Pattyn, A.L. Hubbard, and D. Floricioiu. 2012. The response of Petermann Glacier, Greenland, to large calving events, and its future stability in the context of atmospheric and oceanic warming. Journal of Glaciology 58 (208): 229-239.

Rignot, E. 1996. Tidal motion, ice velocity and melt rate of Petermann Gletscher, Greenland, measured from radar interferometry. Journal of Glaciology 42 (142): 476-485.

The Ice Shelf of Petermann Gletscher, North Greenland and its ocean below: Introductions

“In 1921 owing to starvation I had to go directly from Cape Heiberg-Juergensen to our cache at Cape Agassiz … during this journey the greater part of the glacier was mapped.” — Lauge Koch, 1928

Traveling by dog sled, Geologist Lauge Koch mapped Petermann Gletscher in 1921 after he and three Inuit companions crossed it on a journey to explore northern North Greenland. They discovered and named Steensby, Ryder, and H.C. Ostenfeld Glaciers that all had floating ice shelves as does Petermann (Ahnert, 1963; Higgins, 1990). In Figure 1 I reproduce the historic map of Koch (1928) that also contains his track in in 1917 and 1921 both across the terminus and across its upstream ice stream. In 1921 all four starved travelers returned safely after living off the land. Four years earlier, however, they were not so lucky: two traveling companions died on a similar journey in 1917 (Rasmussen, 1923).

Maps of Petermann Gletscher by Lauge Koch from 1917 and 1921 dog sleds and 2015 from MODIS-Terra.

Only 20 years after Lauge Koch’s expeditions by dog sled, air planes and radar arrived in North Greenland with the onset of the Cold War. The Arctic Ocean to the north became a battle space along with its bordering land and ice masses of northern Greenland, Ellesmere Island, Canada, Alaska, and Siberia. Weather stations were established in 1947 at Eureka by aircraft and in 1950 at Alert by US icebreaker to support military aviation (Johnson, 1990). In 1951 more than 12,000 US military men and women descended on a small trading post called Thule that Knud Rasmussen and Peter Freuchen had established 40 years earlier to support their own and Lauge Koch’s dog-sled expeditions across Greenland (Freuchen, 1935). “Operation Blue Jay” built Thule Air Force Base as a forward station for fighter jets, nuclear armed bombers, and early warning radar systems. The radars were to detect ballistic missiles crossing the Arctic Ocean from Eurasia to North America while bombers were to retaliate in case of a nuclear attack from the Soviet Union.

An F-102 jet of the 332d Fighter-Interceptor Squadron at Thule AFB in 1960. [Credit: United States Air Force]

An F-102 jet of the 332d Fighter-Interceptor Squadron at Thule AFB in 1960. [Credit: United States Air Force]

About another 60 years later, the jets, the bombers, and the communist threat were all gone, but the Thule Air Force Base is still there as the gateway to North Greenland. It is also the only deep water port within a 1,000 mile radius where US, Canadian, Danish, and Swedish ships all stop to receive and discharge their crews and scientists. Since 2009 Thule AFB also serves as the northern base for annual Operation IceBridge flights over North Greenland to map the changing ice sheets and glaciers.

The establishment of military weather stations and airfields in the high Arctic coincided with the discovery of massive ice islands drifting freely in the Arctic Ocean. On Aug.-14, 1946 airmen of the 46th Strategic Reconnaissance Squadron of the US Air Force discovered a moving ice islands with an area of about 200 square that was kept secret until Nov.-1950 (Koenig et al, 1950). Most of these ice islands originated from rapidly disintegrating ice shelves to the north of Ellesmere island (Jeffries, 1992; Copland 2007), however, the first historical description of an ice islands from Petermann Gletscher came from Franz Boas in 1883 who established a German station in Cumberland Sound at 65 N latitude and 65 W longitude as part of the first Polar Year.

Petermann Ice Island of 2012 at the entrance of Petermann Fjord. The view is to the north-west with Ellesmere Island, Canada in the background. [Photo Credit: Jonathan Poole, CCGS Henry Larsen]

Petermann Ice Island of 2012 at the entrance of Petermann Fjord. The view is to the north-west with Ellesmere Island, Canada in the background. [Photo Credit: Jonathan Poole, CCGS Henry Larsen]

Without knowing the source of the massive tabular iceberg the German physicist Franz Boas reported detailed measurements of ice thickness, extend, and undulating surface features of an ice island in Cumberland Sound that all match scales and characteristics of Petermann Gletscher (Boas, 1885). These characteristics were first described by Dr. Richard Croppinger, surgeon of a British Naval expedition in 1874/75 (Nares, 1876). Dr. Croppinger identified the terminus of Petermann Gletscher as a floating ice shelf when he noticed vertical tidal motions of the glacier from sextant measurements a fixed point (Nares, 1876). His observations on tides were the last until a group of us deployed 3 fancy GPS units on the glacier last summer.

These fancy GPS receivers give centimeter accuracy vertical motions at 30 second intervals. Here is what the deployment of 3 such units in August of 2015 gives me:

Vertical (top) and horizontal (bottom) motion of Petermann Gletscher from GPS referenced to a GPS base station on bed rock at Kap Schoubye. Note the attenuation of the tide from 26 km sea ward of the grounding line (red) to at the grounding line (black) and 15 km landward of the grounding line (blue). The horizontal location motion has the mean motion removed to emphasize short-term change over the much, much larger forward motion of the glacier that varies from about ~700 (black) to ~1250 meters per year (red).

Vertical (top) and horizontal (bottom) motion of Petermann Gletscher from GPS referenced to a GPS base station on bed rock at Kap Schoubye. Note the attenuation of the tide from 26 km sea ward of the grounding line (red) to at the grounding line (black) and 15 km landward of the grounding line (blue). The horizontal location motion has the mean motion removed to emphasize short-term change over the much, much larger forward motion of the glacier that varies from about ~700 (black) to ~1250 meters per year (red).

We have indeed come a far way during the last 150 years or so. Mapping of remote landscape and icescape by starvation and dog-sled has been replaced by daily satellite imagery. Navigation by sextant and a mechanical clock has been replaced by GPS and atomic clock whose errors are further reduced by a local reference GPS. These fancy units and advanced data processing allow me to tell the vertical difference between the top of my iPhone sitting on a table in my garden from the table.

Working at in the garden at home preparing for field work.

Working at in the garden at home preparing for field work near Petermann Fjord.

P.S.: This is the first in a series of essays that I am currently developing into a peer-reviewed submission to the Oceanography Magazine of the Oceanography Society. The work is funded by NASA and NSF with grants to the University of Delaware.

Ahnert, F. 1963. The terminal disintegration of Steensby Gletscher, North Greenland. Journal of Glaciology 4 (35): 537-545.

Boas, F. 1885. Baffin-Land, geographische Ergebnisse einer in den Jahren 1883 und 1884 ausgeführten Forschungsreise. Petermann’s Mitteilungen Ergänzungsheft 80: 1-100.

Copland, L., D.R. Mueller, and L. Weir. 2007. Rapid loss of the Ayles Ice Shelf, Ellesmere Island, Canada. Geophysical Research Letters 34 (L21501): doi:10.1029/2007GL031809.

Freuchen, P. 1935. Arctic adventures: My life in the frozen North. Farrar & Rinehard, NY, 467 pp.

Higgins, A.K. 1990. North Greenland glacier velocities and calf ice production. Polarforschung 60 (1): 1-23.

Jeffries, M. 1992. Arctic ice shelves and ice islands: Origin, growth, and disintegration, physical characteristics, structural-stratigraphic variability, and dynamics. Reviews of Geophysics 30 (3):245-267.

Johnson, J.P. 1990. The establishment of Alert, N.W.T., Canada. Arctic 43 (1): 21-34.

Koch, L., 1928. Contributions to the glaciology of North Greenland. Meddelelser om Gronland 65: 181-464.

Koenig, L.S., K.R. Greenaway, M. Dunbar, and G. Hattersley-Smith. 1952. Arctic ice islands. Arctic 5: 67-103.

Münchow, A., K.K. Falkner, and H. Melling. 2015. Baffin Island and West Greenland current systems in northern Baffin Bay. Progress in Oceanography 132: 305-317.

Münchow, A., L. Padman, and H.A. Fricker. 2014. Interannual changes of the floating ice shelf of Petermann Gletscher, North Greenland, from 2000 to 2012. Journal of Glaciology 60 (221): doi:10.3189/2014JoG13J135.

Nares, G. 1876. The official report of the recent Arctic expedition. John Murray, London,

Rassmussen, K., 1921: Greenland by the Polar Sea: the Story of the thule Expedition from Melville Bay to Cape Morris Jessup, translated from the Danish by Asta and Rowland Kenney, Frederick A. Stokes, New York, NY, 327 pp.

Mapping North Greenland 100 years ago

Living off the land, Greenland’s early explorers ate their dogs, fungi, and roots of plants a few inches high to not starve to death. There is nothing romantic in the detailed reports of Knud Rasmussen, Peter Freuchen, and Lauge Koch that mapped in much detail coastlines, glaciers, and fjords of North Greenland between Thule in the west and Independence Fjord in the east. These Danes worked and lived closely with Inuit hunters and their families at what still is the northern edge of where a small number of people can survive by hunting seals, walrus, whales, and polar bears on the ice and musk ox, reindeer, and rabbits on land. Most people did not live as long and as well as we do now, because life and food were always in short supply.

Ascent of the Inland ice in April 1912 as the First Thule Expedition starts from Clemens Markham's Glacier to Independence Fjord. All 4 explorers returned, but only 8 of the 54 dogs did.

Ascent of the Inland ice in April 1912 as the First Thule Expedition starts from Clemens Markham’s Glacier to Independence Fjord. All 4 explorers returned, but only 8 of the 54 dogs did.

I am reading the reports of the First Thule Expedition of 1912 (4 people), the Second Thule Expedition of 1917 (7 people), and the Bicentenary Jubilee Expedition of 1921 (4 people). Each person had its own dog sled team with 10-14 dogs per team. Knud Rasmussen and Peter Freuchen with Uvdloriaq and Inukitsoq successfully crossed the ice sheet in 1912 from east to west and back. Only 5 of the 7 members of the Second Thule Expedition returned, because Greenlander Hendrik Olsen disappeared while hunting wolves which may have killed him and the Swedish scientist Dr. Thorild Wulff starved to death when he gave up walking as witnessed by Lauge Koch and Inuit Nasaitsordluarsuk and Inukitsoq.

Map detail of Inglefield Land with tracks from Second Thule Expedition after leaving the ice sheet, from Rasmussen (1923). Humboldt Glacier is on the right with Kane Basin to the top.

Map detail of northern Inglefield Land with tracks from Second Thule Expedition after leaving the ice sheet with the location of Dr. Wulff’s death. Humboldt Glacier is on the right with Kane Basin to the top. From Rasmussen (1923).

This last death cast a life-long spell on Lauge Koch who never forgave Knud Rasmussen and Peter Freuchen for insisting on a formal Court of Inquiry in local Greenland and not remote Denmark to clear Lauge Koch of any wrong-doing. Both believed that Koch had acted properly when he choose to live and walk and not starve with Wulff, but they felt that local Inuit witnesses and local knowledge in Greenland would make the legal task to clear Koch easier sooner than a more removed Court in Denmark.

Knud Rasmussen (right) and Lauge Koch (left). [Photo: Holger Damgaard, National Library of Denmark.

Knud Rasmussen (right) and Lauge Koch (left). [Photo: Holger Damgaard, National Library of Denmark.

The Freuchen family on a visit to Denmark: Naravana, Pipaluk, Peter, and Mequsaq [Source: Freuchen, P., 1953: Vagrant Viking. Julian Messner Inc., NY, 312 pp.]

The Freuchen family on a visit to Denmark: Naravana, Pipaluk, Peter, and Mequsaq [Source: Freuchen, P., 1953: Vagrant Viking. Julian Messner Inc., NY, 312 pp.]

These Danish expeditions represent the second phase of exploration of North Greenland after the quest of national glory to reach the farthest north by British and Americans was settled when Robert Peary claimed to have reached the North Pole in 1909. The many American and English expeditions through Nares Strait from about 1853 (Elisha Kane) had relied on native guides, hunters, and polar skills, but the sheer number of whites and their massive material wealth change both local cultures and wildlife. For example, the early Europeans and American explorers provided guns and new technologies which were traded for furs, clothing, and local knowledge of survival. In return Inuit families provided food, clothing, and native polar technologies. These often proved crucial for survival as demonstrated by Joe Eberling and Hans Hendrik with their families who kept 18 people alive for 6 months in 1873 when their party of British and German men was stranded on an ice floe drifting more than 1800 miles to the south until they were picked up by a whaling ship off Labrador.

After the “Imperial” expeditions ended with the “conquest of the North Pole” in 1909, the local Inuit were left without contact to southern material goods such ammunition for their guns until Knud Rasmussen and Peter Freuchen privately founded the Thule Trading Post in Westenholme Fjord. Their goal was to set up a base to support their aspiration to explore and map northern Greenland via small expeditions and to show a link between Denmark and the people living in what was then called the Thule district of Greenland. Their choice of location was excellent and even today, Thule is still the hub to get to northern Greenland by ship or by air. I traveled through Thule in 2003, 2006, 2007, 2009, 2012, and 2015 as I boarded US, Canadian, or Swedish icebreaker at this only deep water north of the polar circle outside Scandinavia.

Inner section of Westenholme Fjord to the north-east of Thule AFB as seen on the descent from Dundas Mountain during sunset on Sept.-2, 2015,

Inner section of Westenholme Fjord to the north-east of Thule AFB as seen on the descent from Dundas Mountain during sunset on Sept.-2, 2015,

Peter Freuchen, Lauge Koch, and Knud Rasmussen were all in their 20ies and 30ies when they traveled across a harsh, unvisited, and at times beautiful landscape. Despite local help, skill, and knowledge to adapt to this environment, Greenland almost killed them by starvation or accident as it did to some of their companions. They all were excellent writers and communicators who found the moneys to pay for their adventures in creative ways. Knud died young in 1933 at age 54 in Copenhagen while Peter buried his Inuit wife Navarana in 1921 when he was only 35 years old, but lived another 36 years. Lauge Koch became an international academic authority on the geology and geography of Greenland until he died at age 72 in 1964. They all lived rich, admired, and controversial lives with their writing, their maps, their loves, and above all their frail humanity.

Maps of North Greenland before (top) and after (bottom) the First and Second Thule Expeditions from Rasmussen (1923).

Maps of North Greenland before (top) and after (bottom) the First and Second Thule Expeditions from Rasmussen (1923).

Freuchen, P., 1953: Vagrant viking, my life and adventures, Julian Messner, Inc. New York, NY, 312 pp.

Hendrik, H, 1878: Memoirs of Hans Hendrik, the Arctic traveler serving under Kane, Hayes, Hall, and Nares 1853-1876, reprinted in Cambridge University Press, Cambridge, UK, 100 pp.

Koch, L., 1926: Report on the Danish Bicentenary Jubilee Expedition north of Greenland 1920-23, 232 pp.

Rasmussen, K., 1912: Report of the First Thule Expedition 1912.

Rasmussen, K., 1923: Greenland by the Polar Sea: The story of the Thule Expedition from Melville Bay to Cape Morris Jesup, Frederick A. Stokes Company, New York, NY, 328 pp.

Ghosts of Discovery Harbor: Digging for Data

Death by starvation, drowning, and execution was the fate of 19 members of the US Army’s Lady Franklin Bay Expedition that was charged in 1881 to explore the northern reaches of the American continent. Only six members returned alive, however, they carried papers of tidal observations that they had made at Discovery Harbor at almost 82 N latitude, less than 1000 miles from the North Pole. Air temperatures were a constant -40 (Fahrenheit or Celsius) in January and February. While I knew and wrote of this most deadly of all Arctic expeditions, only 2 days ago did I discover a brief 1887 report in Science that a year-long record of hourly tidal observations exist. How to find these long forgotten data?

My first step was to search for the author of the Science paper entitled “Tidal observations of the Greely Expedition.” Mr. Alex S. Christie was the Chief of the Tidal Division of the US Coast and Geodedic Survey. He received a copy of the data from Lt. Greely. His activity report dated June 30, 1887 confirms receipt and processing of the data, but he laments about “deficient computer power” and requests “two computers of standard ability preferable by young men of 16 to 20 years.” Times and language have changed: In 1887 a computers was a man hired to crunch numbers with pen and paper.

Data table of 15 days of hourly tidal sea level observations extracted from Greely (1888).

Data table of 15 days of hourly tidal sea level observations extracted from Greely (1888).

While somewhat interesting, I still had to find the real data shown above, but further google searches of the original data got me to the Explorer’s Club in New York City where in 2003 a professional archivist, Clare Flemming, arranged and described the “Collection of the Lady Franklin Bay Expedition 1881-1884.” This most instructive 46 page document lists the entire collection of materials including Series III “Official Research” that consists of 69 folders in 4 Boxes. Box-4 File-15 lists “Manuscript spreadsheet on Tides, paginated. Published in Greely (1888), 2:651-662” as well as 3 unpublished files on tides and tide gauges. With this reference, I did find the official 1888 “Report on the United States Expedition to Lady Franklin Bay” of the Government Printing Office as digitized from microfiche as

https://archive.org/details/cihm_29328

which on page 641 shows the above table. There are 19 more tables like it, but at the moment I have digitized only the first one. Unlike my colleagues at the US Coast and Geodedic Survey in 1887, I do have enough computer power to graph and process these 15 days of data in mere seconds, e.g.,

Hourly tidal observations at Discovery Harbor taken for 15 days by Greely in 1881 and Peary in 1909.

Hourly tidal observations at Discovery Harbor taken for 15 days by Greely in 1881 and Peary in 1909.

A more technical “harmonic” analyses reveals that Greely’s 1881 (or Peary’s 1909) measured tides at Discovery Harbor have amplitudes of about 0.52 m (0.59) for the dominant semi-diurnal and 0.07 m (0.12) for the dominant diurnal oscillation. My own estimates from a 9 year 2003 to 2012 record gives 0.59 and 0.07 m for semi-diurnal and diurnal components. This gives me confidence, that both the 1881 and 1909 data are good, just have a quick look at 1 of the 9 years of data I collected:

Tidal sea level data from a pressure sensor placed in Discovery Harbor in 2003. Each row is 2 month of data starting at the top (August 2003) and ending at the bottom (July 2004).

Tidal sea level data from a pressure sensor placed in Discovery Harbor in 2003. Each row is 2 month of data starting at the top (August 2003) and ending at the bottom (July 2004).

There is more to this story. For example, what happened to the complete and original data recordings? Recall that Greely left Discovery Harbor late in the fall of 1883 after supply ships failed to reach his northerly location two years in a row. This fateful southward retreat from a well supplied base at Fort Conger and Discovery Harbor killed 19 men. Unlike ghostly Cape Sabine where most of the men perished, Discovery Harbor had both local coal reserves and musk ox in the nearby hills that could have provided heat, energy, and food for many years.

It amazes me, that a 1-year copy of tidal data survived the death march of Greely’s party. It took another 18 years for the complete and original records to be recovered by Robert Peary who handed them to the Peary Arctic Club which in 1905 morphed into Explorer’s Club of New York City. I suspect (but do not know), that these archives contain another 2 years of data that nobody but Edward Israel in 1882/83 and the archivist in 2003 laid eyes on. Sergeant Edward Israel was the astronomer who collected the original tidal data. He perished at Cape Sabine on May 29, 1884, 25 years of age.

Edmund Israel, astronomer of the Lady Franklin Bay Expedition of 1881-1884.

Edmund Israel, astronomer of the Lady Franklin Bay Expedition of 1881-1884.

References:

Christie, A.S., 1887: Tidal Observations of the Greely Expedition, Science, 9 (214), 246-249.

Greely, A.W., 1888: Report on the Proceedings of the United States Expedition to Lady Franklin Bay, Grinnell Land, Government Printing Office, Washington, DC.

Guttridge, L., 2000: The ghosts of Cape Sabine, Penguin-Putnam, New York, NY, 354pp.

Below Petermann Glacier: The First 100 Days

I am still stunned to see data coming to me hourly from below a glacier in northern Greenland while I sip my breakfast coffee. Each and every day for the last 100 days I got my data fix from the Ocean Weather Station that was born 100 days ago. Every morning at 8:15 the station sends me data from 5 ocean sensors below the glacier. A year ago I did not even know that I would be going to northern Greenland with the Swedish icebreaker I/B Oden in the summer of 2015, never mind that we would be able to pull off the engineering challenge to set up the first and only ocean observing system of Greenland. Today, I am over-joyed to report, we got 100 days of data.

IMG_3029

University of Delaware PhD student Peter Washam at the Ocean-Weather station on Petermann Gletscher after final installation 2015-Aug.-20, 17:00 UTC at 80 39.9697 N and 60 29.7135 W.

It all started when a French PhD student approached me at a scientific meeting in San Francisco last December. Céline is a now a doctor of oceanography, but at the time she was not. At the meeting Dr. Céline Heuzé of the University of Gothenburg in Sweden asked me for data and insights on how the ocean circulation in Nares Strait worked, so that she could connect results from planned field work in northern Greenland to her science interests in the Labrador Sea more than 1000 miles to the south. She also introduced me to Dr. Anna Wåhlin and the three of us got very excited about Petermann Fjord, Sweden, and polar oceanography. Here we are in Sweden preparing and off Greenland working:

A few weeks prior the US government and Sweden had just agreed to work together on a joint expedition to Petermann Fjord in northern Greenland. Friends at Oregon State University needed a ship to collect data with which to reconstruct and understand changes of the land- sea-, and ice-scape of North Greenland during the last 10,000 to 50,000 years. They wanted to uncover where past glaciers were located and where sea level was at that time. For this, they needed many sediment cores from the adjacent ocean, fjord, and below the floating glacier. Today this glacier is as thick as the Empire State Building in Manhattan is high. The British Antarctic Survey (BAS) agreed to drill the holes, collect the sediment samples, and take a profile of ocean properties from below the glacier ice to the bottom of the ocean. They estimated it would take about 5 days to drill each hole. Our idea was to use these holes to keep sensors, computers, and satellite phones in place to collect hourly data into the future as long as possible … 100 days so far.

After the Dec.-2014 San Francisco meeting we decided to use these holes to measure ocean temperature, salinity, and pressure for as long as the batteries would last, about 3-4 years, but I had neither money, cables, data logging computers, nor satellite phones to do any of this, only the ocean sensors. When I told Keith Nicholls of BAS about the idea and my predicament, he said that he could find some computers and satellite phones from experiments he had done in Antarctica. I then said that I would organize cables, a weather station, and some funds to pay for it.

A crowd-funding experiment in February failed to generate funds, but NASA came to the rescue by opening a way to compete for the needed $60,000 to cover the cost of hardware, travel, and satellite phone charges. The funds allowed us to ship about 1200 pounds of gear from Delaware to Sweden where it had to be loaded onto the ship in May of 2015. We did not have much time to built the system and had no time left to test it. Two drums of cable arrived with only 5 hours to spare before the ship left Sweden in June for Greenland. We met the ship in Thule, Greenland in July.

Fast-forward to the 20th of August 2015 when our ocean observing system went into the salty ocean waters below Petermann Gletscher. The surface weather station with satellite connections was deployed 10 days earlier to test satellite communications and collect weather data for Oden’s extensive helicopter flight operations on and around the glacier. It included a rushed visit by a large team from CBS News 60 Minutes who were flown and shown all over the place. We last saw the station during 24 hours of day light on 27th August when we calibrated the wind sensors, but to me the daily satellite phone call of the station with new data is a sign of life from an ocean outpost that survived another day in the total darkness of the polar night. It draws energy from two car batteries that run even at the -36 degree Centigrade (-33 F).

AWS

First 100 days of ocean and weather observations from the University of Delaware Ocean Weather Station on Petermann Gletscher, Greenland. Panels show (from bottom to top) time series of 1. battery voltage, 2. ocean (red) and air (black) temperatures, 3. wind speed, 4. wind direction, 5. glacier movement, and 6. atmospheric pressure. Time is given in year-day, Nov.-28 is Day-332. The sun set on Day-290 or Oct.-17.

New data are posted at

http://ows.udel.edu

which over the next few weeks we will develop into a web-site to distribute the daily observations to everyone. I am most thankful to many of scientists, engineers, technicians, sailors, and women in England, Sweden, and the United States of America, but this Thanks-Giving weekend I am grateful to the men and women of a great nation that gave me a place to study, work, and live doing while exploring ocean and now glacier physics as well.

EDIT: I just discovered this 7 minute video on our expedition, credits go to Saskia Madlener at 77th Parallel Productions: