1. Introduction
The British Admiralty and Royal Society jointly sponsored James Cook's 1772–1775 circumpolar Antarctic cruise on the HMS Resolution. Although the cruise began with two ships, with Tobias Furneaux commanding the Adventure, on 30 October 1773, they became permanently separated. During the austral spring and summers, the Resolution made five traverses into the sea ice and iceberg-covered regions of the Antarctic Ocean, then spent its austral winters in more temperate latitudes. On these traverses, Cook observed hundreds of icebergs.
One of the Admiralty's instructions to Cook was to investigate an earlier discovery. On 1 January 1739, Lozier Bouvet on the ships Aigle and Marie (Eagle and Mary) of the French East India Company observed what he thought was land in the South Atlantic at 54.0°S, 11.3°E. Bouvet named this feature Cape Circumcision, after the 1 January date of the Feast of the Circumcision. Although Bouvet may have seen what is now Cape Circumcision on Bouvet Island at 54.0°S, 3.3°E or 530 km west of his recorded position, Cook was to search the region around 11.3°E and investigate whether this observation was part of a much larger land mass (Cook, Reference Cook1777a, Reference Cook1777b, 24, 52).
On the Resolution, Cook used the new Larcum Kendall K1 watch. This was an exact copy of the Harrison H4 watch that in combination with sextant observations of the sun elevation, allowed longitude to be determined with an accuracy of 6–19 km (3–10 nm), or at 60°S, to an accuracy of 0.1–0.3 degrees (Sobel, Reference Sobel2005; Skullern, Reference Skullern2016). Cook took great care of the K1. When it was removed from storage to be used or wound, the commander, first lieutenant and astronomer, or their designated alternates, had to be present. Other methods for longitude determination included measurement of the apparent size of the moon, for which purpose the crew included an astronomer, William Wales.
Determination of position from either the K1 or astronomical observations required clear skies, so that during bad weather, gaps occurred in their cruise track. Otherwise, Cook and Wales determined the ship's position at ~24 h intervals, where the interval between positions could be as large as 250 km. At these positions, Cook recorded the number of icebergs he saw, and in some cases the size, which he gave as the iceberg circuit-length or circumference. On 24 January 1774, Cook recorded his largest iceberg, which he described as ‘a very large ice-island…not less than three to four miles [6 to 8 km] in circuit (Cook, Reference Cook1777a, 267)’.
Cook rewrote his journal for publication in terms of ‘civil time’, where days run midnight to midnight, instead of the Royal Navy ‘nautical time’, where days run noon to noon (Cook, Reference Cook1777a, xxxv). Wales kept his journal in nautical time and recorded all navigational data with additional observations of ice conditions (Wales, Reference Wales1775). His handwritten logbook is available on-line from the Greenwich Observatory. Because of their different definitions of a day, Wales's morning of 29 January corresponds to Cook's morning of 30 January.
Part of Cook's success came from his discovery that the icebergs could supply sufficient fresh water for his long traverses into the ice. On 14 December 1772, at the beginning of his first traverse in the Weddell Sea, Cook recovered small pieces of glacier ice from the sea and found that they yielded fresh water (54.8°S, 21.5°E). On 8 January 1773, Cook deployed three boats, and in ~6 h, recovered enough ice from an iceberg to yield ‘fifteen tons of good fresh water’. Cook realized that icebergs could supply his fresh water needs, and that ‘I did not doubt of getting more whenever we were in want. I therefore, without hesitation, directed our course more to the south… (Cook, Reference Cook1777a, 88)’. Figure 1 shows a watercolor of the two ships and the ice recovery by the artist on the Resolution, William Hodges.
Watercolor by William Hodges, dated 4 January 1773, with the caption The Resolution and Adventure, taking on ice for water, Latitude 61 S. The illustration corresponds to the ice recovery described in Cook's log on 8 January 1773 at 61.2°S, 31.8°W. For scale, the Resolution measures 100 m at the waterline. The image is out of copyright and courtesy of the Mitchell Library, State Library of New South Wales (Mitchell Library, 2022).
This study discusses observations of Antarctic icebergs from Cook on the HMS Resolution, Halley on the HMS Paramore and Riou on the HMS Guardian, and includes Bouvet's observation of Cape Circumcision on the Aigle and Marie that helped inspire Cook's voyage. Cook's observations make up 95% of the total. Comparison of their size distribution with modern data, and their spatial distribution with the trajectories of contemporary satellite-tracked icebergs from the Alfred Wegener Institute (AWI) and the Brigham Young University/National Ice Center (BYU/NIC) shows that except for the location of the Guardian icebergs, the modern and historic datasets agree. The study then describes Cook's five traverses into the eastern Weddell Sea, the Indian Ocean, the Ross Sea, the Amundsen Sea and the western Weddell Sea. For the Guardian outliers, the application of a drift and fracture model to the BYU/NIC trajectories extends them to the positions of the Guardian icebergs, so that modern observations and theory explain all the historic ship observations. In the conclusions, notable results include Cook's transect in the Indian Ocean through the iceberg plume that exits the coast to the east of the Amery Ice Shelf, and his attainment in the Amundsen Sea of his furthest south, where the Resolution was the first ship to reach the continental shelf of the Amundsen Sea Embayment (ASE) which contains the terminuses of the Pine Island and Thwaites Glaciers. This achievement is a remarkable precursor to the International Thwaites Glacier Collaboration (ITGC) that in the same location in 2018, began its fieldwork 244 years later.
2. Datasets
2.1 HMS Resolution
The lead author extracted Cook's observations of the number of icebergs versus position and date along his five traverses from a line-by-line search of a downloadable version of Cook (Reference Cook1777a, Reference Cook1777b). Whenever possible, Cook (Reference Cook1777a, Reference Cook1777b) recorded his position plus his observations of icebergs, which he referred to in terms such as ‘ice islands’, ‘ice isles’ and ‘hills of ice’. This paper supplements Cook's observations by inclusion of one observation from Wales's (Reference Wales1775) handwritten logbook. For the subsequent data display (see Fig. 2 below), Cook's and Wales's observations were divided into three categories: no icebergs, one to three icebergs and many icebergs. These were transcribed into the spreadsheet in the Supplementary material that contains the date, position, the iceberg categories and Cook's or Wales's description of each observation. The latitude and longitude are given to 0.1 degrees, which as the previous section discusses, is the best longitude accuracy associated with the Kendall chronometer. Since positions were taken at local noon, and the ship could travel as much as 200 km d−1 with the iceberg observations occurring at any time, the actual iceberg positions were less accurate. The final spreadsheet includes 93 observations from Cook and one from Wales. For quality control, the first draft of these points was plotted on a polar projection, then compared with Cook's cruise plot (Cook, Reference Cook1777a, Plate I), following which outliers were removed, revised and reentered. The entire file was then rechecked against the original texts.
Comparison of the datasets: BYU/NIC in red, AWI in orange, Halley, Bouvet and Riou observations in black and Cook's cruise tracks and data points in blue. His first traverse of the Weddell Sea is a solid line; his second is dotted. For Cook, open circles mean no icebergs; small closed circles, one to three icebergs; larger closed circles, many icebergs. The circled point on 8 January 1773 marks where Cook collected fresh water from an iceberg and of Hodges's watercolor. Also marked are Cook's three crossings of the Antarctic circle, his farthest south and the sea-ice and iceberg tongue in the Weddell Sea. The dashed lines between 45°S and 60°S show the boundaries of the Antarctic Circumpolar Current (ACC). The dotted circle is the Antarctic Circle. The latitude–longitude box (62°S–68°S, 3°W–12°E) in the Weddell Sea shows the location of the Maud Rise Polynya.
2.2. Other historic ship observations
During 1700–1799, and in addition to Lozier Bouvet's discovery on the Aigle and Marie of Cape Circumcision, Edmond Halley on the HMS Paramore and Edward Riou on the HMS Guardian provided five more iceberg observations that the spreadsheet includes. Although these ships recorded few icebergs, Halley observed the largest, the Bouvet discovery was an inspiration for Cook's voyage and Riou's encounters show the importance of fractures in the determination of iceberg trajectories.
2.2.1 HMS Paramore
On 1 February 1700, Edmond Halley, who determined his longitude from dead reckoning, reached a point just north of the undiscovered South Georgia Island. At this position, Halley encountered three tabular icebergs and provided what may be their first sketches and written descriptions (Thrower, Reference Thrower1981). The largest of these icebergs which Halley named ‘B’ had a 60 m freeboard and a 9 km waterline length. He then sailed north, encountering a few smaller icebergs in fog. For all the ships, his iceberg ‘B’ was the largest observed.
2.2.2 HMS Guardian
Between 21 and 27 December 1789, Captain Edward Riou of the HMS Guardian, a supply ship en route to the new Australian colony, was surprised to see several icebergs 2100 km southeast of Cape Town at about 44°S, or well north of Cook's observations (Riou, Reference Riou1790; Dickson, Reference Dickson2012). On 22 December, Riou observed two icebergs, where the first was saddle-shaped and measured ~10 m high and 300 m long at the waterline, with a similarly sized iceberg observed from the masthead (Riou, Reference Riou1790, 4–5). On this day, Riou reported that the air temperature remained between 50° and 60°F (10–15°C), suggesting that the seawater surface temperature was above freezing.
On Christmas Eve 1789, Riou observed a third iceberg with a waterline length of ~200 m and hummocks at each end, the larger 60 m high, the smaller 15 m high (Riou, Reference Riou1790, 7–13). In the late afternoon, Riou deployed small boats to this iceberg to recover ice for fresh water. From Riou (Reference Riou1790, 9), as the boats approached, tonnes of ice fell from the large hummock, providing ‘convincing proof of [its] rapid decay…’. About an hour after completing this task, in the early evening and heavy fog, the Guardian collided with a fourth iceberg, which Riou describes as ‘a body of ice full twice as high as our masthead, showing itself through the thickest fog I ever witnessed (Dickson, Reference Dickson2012, 23)’. Given a mast height of ~30 m, this implies an ice height of ~60 m. Because of the fog, no additional information exists on the size of this iceberg.
The sailing master of the ship, Thomas Clements, stated that while the ship turned away from the iceberg, it collided stern-first with ‘a piece of ice, which projected out from the main body underwater… (Dickson, Reference Dickson2012, 31)’. The incident ocean swell drove the Guardian onto the underwater projection with sufficient force that its rudder was torn off and bottom severely damaged, following which it ran aground.
As Wagner and others (Reference Wagner2014) show, this underwater ice foot results from wave melting. If the ocean is above freezing, the waves carry heat toward the iceberg, cutting a notch at the waterline. After the notch grows in a few meters, the ice above the waterline sloughs off, while the underwater foot remains. If this foot grows large enough, its buoyant torque will fracture the iceberg, a process called the ‘footloose’ mechanism (Wagner and others, Reference Wagner2014). For 5 or 6 min, the Guardian remained grounded on the foot, during which time Riou and Clements feared that the overhanging ice would fall and destroy the ship. The ship then broke free and moved clear of the iceberg (Riou, Reference Riou1790, 19; Dickson, Reference Dickson2012, 23, 31).
Following the collision, about half of the 124 crew, passengers and convicts abandoned ship, while the rest remained onboard with Riou. On 27 December 1789, at 43.2°S, 45°W, Riou observed his last iceberg. Because Riou's chronometers were stolen in the chaos surrounding the collision, the longitude given here and in the spreadsheet is from dead reckoning. Then in an amazing feat and despite the severe damage, Riou sailed the hulk on an irregular course 2500 km back to Cape Town, arriving 60 d after the collision on 22 February 1790 (Dickson, Reference Dickson2012).
2.3 Modern iceberg observations
2.3.1 Brigham Young University/National Ice Center (BYU/NIC)
The BYU/NIC dataset began in July 1978 and continues through the present, with most of its data collection occurring since 1992 (Stuart and Long, Reference Stuart and Long2011; Budge and Long, Reference Budge and Long2018). The BYU part of the dataset uses low-resolution satellite scatterometer radars to track icebergs. Volume scattering from the radar signal penetrating into the firn makes the icebergs much brighter than either the ocean surface or sea ice. During the austral summer, when meltwater forms on the iceberg surface, the contrast disappears, leading to gaps in the trajectories. The backscatter measurements are processed onto polar stereographic grids with 8.9, 4.2 or 2.2 km pixels, depending on the sensor. Since it takes several pixels to unambiguously identify an iceberg, the smallest iceberg that can be tracked has a length of 5–10 km. The NIC part of the data consists of iceberg positions derived from visible, infrared and radar satellite observations. These are used to check the scatterometer positions or occasionally to fill in missing data (Budge and Long, Reference Budge and Long2018). Since Cook's largest iceberg had a circumference of ~8 km, corresponding to a 3 km diameter, it would have been too small for the scatterometer to observe.
2.3.2 Alfred Wegener Institute (AWI)
The AWI dataset contains the results from the January 1999 to January 2003 deployment of satellite transponders from the R/V Polarstern onto 52 icebergs in the Weddell Sea. These buoys reported GPS positions at daily intervals via ARGOS. Most of these icebergs had lengths between 100 and 1500 m, and freeboards between 10 and 70 m, with a few much larger (Schodlok and others, Reference Schodlok, Hellmer, Rohardt and Fahrbach2006). Their deployments used two types of buoys. In the first year, the transponders were mounted in sealed tubes that were 2 m tall with a 20 cm diameter, with additional floatation attached. Because of their large number of batteries, the German environmental protection agency (Umwelt Bundesamt) required that if these buoys melted free, they would be able to float out of the Antarctic treaty zone. The second type was 1.8 m tall with a 20 cm diameter and had a positive buoyancy without an additional float. All buoys were buried halfway into the iceberg with an attached meter-square wooden panel at the surface to avoid tilting (Schodlok and others, Reference Schodlok, Hellmer, Rohardt and Fahrbach2006).
3. Results
3.1 Comparison of ship and modern observations
3.1.1 Iceberg sizes
Cook recorded his largest iceberg on 24 January 1774, when he observed ‘a very large ice-island…not less than three to four miles [6 to 7 km] in circuit (Cook, Reference Cook1777a, 267)’. Cook's larger estimate of circumference is equivalent to a 2.4 km diameter iceberg with a 4.4 km2 area. He does not describe encounters with the 100 km scale icebergs, such as icebergs B-15A, C-19A or A-68 that occur within the BYU/NIC dataset.
In their Figure 2 and Table S2, England and others (Reference England, Wagner and Eisenman2020) show the size distribution of icebergs based on their interpretation of the −1.5 power-law dependence of iceberg frequency on area (Tournadre and others, Reference Tournadre, Bouhier, Girard-Ardhuin and Rémy2016). Their table gives this dependence in terms of eight area categories that range from 0.3 to 1000 km2. The four categories with areas ≤10 km2, corresponding to a 3.2 km diameter, account for 92% of the total icebergs. While Halley's iceberg ‘B’ had a 9 km length at its waterline, such that it was the largest iceberg observed from any of the ships and would have been visible in the scatterometer data, Halley provided no estimate of its area. Assuming that the Resolution encountered 1000 icebergs, their Table S2 shows that only seven of these would have areas >1000 km2. The low probability of these giant icebergs is one reason that they were not observed from the ships.
3.2.1 Iceberg trajectories and positions
Figure 2 shows Cook's cruise tracks and iceberg observations in blue, the BYU/NIC trajectories in red, the AWI trajectories in orange, and the Halley, Bouvet and Riou observations in black, where these colors were chosen to make the figure color-blind accessible. An unusual feature of the display is that many of the orange trajectories occur southeast of the red trajectories. Wagner and others (Reference Wagner, Dell and Eisenman2017) provide an explanation. As their analysis and their Figure 7 show, large icebergs, which they define as having length scales >15 km, drift with the ocean currents. Smaller icebergs, which they define as having length scales <1.5 km, continue to drift with the currents but are more strongly driven by the winds. This size difference roughly corresponds to different iceberg sizes of the two satellite datasets.
Stern and others (Reference Stern, Adcroft and Sergienko2016, Figs 3a–3c) similarly show that as the iceberg length scale increases from 60 m to 1.7 km, the trajectories of the Weddell icebergs shift from the winds carrying them into the central Weddell to the currents keeping them adjacent to the coast. For Halley's iceberg ‘B’, its location north of South Georgia places it within the stream of large icebergs carried by the currents. All this strongly suggests that the red trajectories tend to follow the currents, while most of the orange trajectories follow the winds.
The red BYU/NIC trajectories show there is a dense counterclockwise coastal flow of icebergs around the continent to the Weddell Sea, where the Antarctic Peninsula diverts them to the northeast into a region of the South Atlantic nicknamed ‘Iceberg Alley’. About 90% of the icebergs exit the Antarctic region through this outflow (Stuart and Long, Reference Stuart and Long2011). Of the remainder, 8% exit the Ross Sea, and ~2% leave the coast east of the Amery Ice Shelf at about 90°E. Since the neglect of small icebergs biases these percentages, the actual outflow from the region may be much larger.
3.2 Cook's five traverses
3.2.1 First traverse: Eastern Weddell Sea
After leaving Cape Town, Cook's first traverse began in the Weddell Sea when on 10 December 1772, he saw his first iceberg. Cook ‘judged it to be about 50 feet (15 m) high and half a mile (800 m) in circuit. It was flat at top, and its sides rose in a perpendicular direction (Cook, Reference Cook1777a, 22)’.
On 14 December 1772, Cook encountered a tongue of sea ice and icebergs that blocked his advance south. From Cook's description, ‘…we were stopped by an immense field of low ice; to which we could see no end, either to the east, west, or south. In different parts… were islands, or hills of ice, like those we found floating in the sea… (Cook, Reference Cook1777a, 24)’. The ship sailed east until on 21 December, it reached the tip of this sea-ice tongue, ‘…having never less than ten or twelve islands in sight (Cook, Reference Cook1777a, 29)’. The Resolution then sailed south until it reached the southern edge of the tongue, turning west on Christmas Day with the goal of reaching the longitude of Cape Circumcision (12.5°E).
The position of this sea-ice tongue is in part determined by the Maud Rise Polynya, which frequently occurs in the austral autumn within the 62°S–68°S, 3°W–12°E box in Figure 2 (Mchedlishvili and others, Reference Mchedlishvili, Spreen, Melsheimer and Huntemann2022). The combination of the winds and ocean circulation drives the warm water upwelling within the polynya, which in late autumn melts the surface ice. From the numerical model of Beckmann and others (Reference Beckmann, Hellmer and Timmerman1999), the polynya is at one of the two centers of the double-cell Weddell gyre, with the other at ~15°W.
From daily passive microwave sea-ice images from National Snow and Ice Data Center (NSIDC), Figure 3 shows that for 14 December 2018, the sea-ice tongue also occurs (NSIDC, 2022). On the figure, the black line is the median ice extent for the same day averaged over 1981–2010. This median line shows the ice extent and the Maud Rise Polynya. The tongue is a transient feature, with its northern boundary determined by the melting ice edge, and its southern boundary by a combination of the receding ice edge and the growing open-water area of the polynya. Relative to Cook's sea-ice tongue, the NSIDC tongue occurs a week to 10 days earlier, with its northern boundary ~500 km south, and its eastern tip ~250 km east.
Passive satellite image of the Antarctic sea-ice extent for 14 December 2018. Sea ice is white, water is light gray, the continent is dark gray. For the same date and the thirty-year period 1981–2010, the black lines show the median ice extent. The open water associated with the Maud Rise Polynya (indicated with arrow) is visible in both the daily and median image (Image courtesy NSIDC).
Given the sea-ice tongue as evidence for a greater ice extent during 1772 in the eastern Weddell Sea, Parkinson (Reference Parkinson1990) examined Cook's other observations of the sea-ice edge, which occurred during his three crossings of the Antarctic Circle. She found that these were either consistent with or even slightly less than the 1970s satellite observations. As Parkinson (Reference Parkinson1990, 7) concludes, given the lack of enhanced sea-ice extents from other regions, the enhanced ice cover that Cook observed is ‘of interest, but …remains unexplained’.
On 8 January 1773, after leaving the tongue, Cook made his critical recovery of fresh water at the position circled in Figure 2, then on 17 January 1773, the Resolution crossed the Antarctic Circle for the first time, where compact sea ice stopped its farther southward movement. The ship was 175 km from land, its closest distance to the continent. It then sailed north on this traverse until on 30 January 1773, Cook reported his last iceberg.
3.2.2 Second traverse: Indian Ocean
On 16 February 1773, the Resolution sailed southeast in the Indian Ocean to encounter a region of enhanced iceberg density. Between 81°E and 97°E, Cook and Wales observed many icebergs in approximately the same location as the BYU/NIC iceberg plume around 90°E in Figure 2. Tournadre and others (Reference Tournadre, Whitmer and Girard-Ardhuin2008, Fig. 6b), from an analysis of altimeter data for November 2004 to December 2005, also found a large concentration of icebergs south of 60°S between 70°E and 120°E.
For this region, Wales (Reference Wales1775) provides a valuable supplement to Cook's description. For 18 February, as marked on Figure 2, when Cook only reported position, Wales (Reference Wales1775, 64) reported ‘many very large islands of ice’. Cook also provides no position or iceberg observations for 19 February, yielding a gap in his observations between 18 and 20 February, corresponding to longitudes 83°E and 91°E, for a separation of 465 km. Although Wales (Reference Wales1775, 64) does not give position data for 19 February, in the morning he reports ‘eight exceedingly large islands of ice’, and in the afternoon, ‘many large islands of ice’. His observation fills the gap in Cook's data and shows that the iceberg coverage remains dense across the plume.
For 20 February 1773 at 91°E, Cook wrote ‘nothing was to be seen but ice islands’. On 23 February at 95°E, Cook said ‘[daylight] only served to increase our apprehensions, by exhibiting to our view those huge islands of ice, which in the night, we had passed without seeing (both quotes from Cook, Reference Cook1777a, 55–56)’. After sailing through the plume, the Resolution encountered few icebergs as it continued east, until 16 March 1773, when it turned north.
3.2.3 Third traverse: Ross Sea
On 8 December 1773, during the next austral summer, the Resolution sailed south along 180° to reach the western Ross Sea, then transited east. As Figure 2 shows, some of the icebergs within this region originated from the vicinity of the Ninnis/Mertz Ice Tongue at about 150°E, others originated directly from the Ross Sea. On 20 December 1773, the ship crossed the Antarctic Circle for the second time. The next morning, Cook wrote ‘The ice islands …were high and rugged, forming at their tops many peaks…many of them were between two and three hundred feet (60–90 m) in height and between two and three miles (4–6 km) in circuit, with perpendicular cliffs or sides, astonishing to behold’. On 24 December at 138°W, Cook wrote ‘we could see near 100 around us’, and on 26 December at 134°E, he saw ‘200 large ice islands (all quotes from Cook, Reference Cook1777a, 254–256)’. On 31 December 1773 at 131°E, the ship turned north, leaving the region on 6 January 1774.
3.2.4 Fourth traverse: Amundsen Sea
On 13 January 1774, the Resolution sailed into the Amundsen Sea. It crossed the Antarctic Circle for the third time, then on 30 January 1774 achieved its farthest south (71.2°S, 106.9°W) on the shelf of the ASE, into which the Pine Island and Thwaites Glaciers discharge. At this position, the water depth was 480 m, and the ship was 10 km south of the shelf break and 400 km north of the present position of the Pine Island Glacier (depth and locations from ETOPO1, Amante and Eakins, Reference Amante and Eakins2009).
A solid wall of pack ice and icebergs confronted the ship, which Cook described as follows: ‘…at eight o'clock [in the morning], we were close to its edge. It extended east and west, far beyond the reach of our sight…Ninety-seven ice-hills were distinctly seen within the field, besides those on the outside, many of them very large, and looking like a ridge of mountains, rising one above another till they were lost in the clouds…(Cook, Reference Cook1777a, 267)’. Wales (Reference Wales1775, 181) helps interpret Cook's description. Wales stated that the morning was foggy and ‘…within this field, which we could not see over, there seemed to run a long ridge of prodigious high mountainous ice, which was probably only a fog-bank’.
Taken together, Cook's and Wales's observations suggest that the apparent rise of the ice into the clouds was an illusion generated by the fog, and not a view of an ice shelf or glacier. In support of this interpretation, Larter and others (Reference Larter2014) show from marine geophysical data that 10 000 years ago, the ice shelves in the embayment were close to their present positions. Also, Graham and others (Reference Graham2022), in their examination of the retreat of the Thwaites Glacier, cite evidence that shows over the past millennia, its retreat rate was 0.01–0.02 km per year, while their work on the Thwaites response to a grounding ridge shows that short periods of rapid retreat of ~2 km per year punctuate this long-term rate. For the last two centuries, they estimate overall rates of 0.3–0.8 km a–1. Both studies suggest that during Cook's visit, the ice shelves in the embayment were at least 200 km south of the Resolution, so that Cook and Wales could not have seen the glaciers. The large number of icebergs that Cook and Wales observed probably originated from calving of the Thwaites and Pine Island Glaciers. After this achievement, the ship turned north, and Cook ceased to record icebergs.
Because of its potentially large contribution to sea-level rise, the Thwaites Glacier is a topic of urgent scientific study. In 2015, the US National Academy of Sciences and the UK Royal Society endorsed a joint 5-year program, the ITGC, that began its fieldwork in 2018 (Scambos and others, Reference Scambos2017; NSIDC, 2018; ITGC, 2022). Thus, for the ASE, the Royal Society endorsed both Cook's expedition and the ITGC, two projects separated by 244 years.
3.2.5 Fifth traverse: Western Weddell Sea
Eleven months later on 3 January 1775, the Resolution left a protected anchorage on Isla de los Estados (Staten Island) in the vicinity of Cape Horn and sailed east into the Weddell Sea. In iceberg-free waters, Cook discovered South Georgia Island, then sailed southeast to discover the South Sandwich Islands. On 28 January 1775 at 60.0°S, 29.3°W, Cook observed his first icebergs on this traverse. Cook stated they were ‘surrounded with a vast number of large ice-islands…[These] were nearly all the same height, and showed a flat even surface…some being two or three miles [4–6 km] in circuit’. From their circumference, these icebergs had diameters of ~2 km. Two days later at 59.5°S, 29.4°W, they ‘…passed one of the largest ice-islands we had seen…’ without recording its size (Cook, Reference Cook1777b, both quotes p. 204).
Figure 2 shows that although the icebergs from Cook's second Weddell traverse lie within the envelope of the BYU/NIC and AWI trajectories, they are displaced to the east. This displacement may be due to Cook's course, where he sailed northeast along the edge of BYU/NIC trajectory envelope, then southeast along the South Sandwich Island arc. It may also result from natural variability, since Cook's traverse provides only a 1-month sample of the iceberg distribution, while the BYU/NIC trajectories provide a multi-decadal sample. Despite this eastern displacement, Cook's icebergs lie within the satellite trajectories.
On 14 February 1775, they crossed the prime meridian and sailed through Bouvet's position for Cape Circumcision, after which Cook concluded that what Bouvet ‘had seen could be nothing but an island of ice, for if it had been land, it is hardly possible we could have missed it (Cook, Reference Cook1777b, 319)’. Finally on 26 February near 30°E, they saw their last iceberg before returning to Cape Town.
4. Reconciliation of the Guardian observations with modern data
The iceberg observations by Halley, Bouvet and Cook agree with modern data. For Cook, this includes the plume of icebergs from east of the Amery Ice Shelf and the iceberg distributions in the Weddell, Ross and Amundsen Seas. Riou's icebergs, however, lie ~1000 km east of the nearest BYU/NIC trajectories. As England and others (Reference England, Wagner and Eisenman2020) show, these can be brought into agreement by extension of the BYU/NIC trajectories by application of a drift model and the footloose mechanism (Wagner and others, Reference Wagner2014).
As Section 2.2.2 describes, the footloose fracture mechanism depends on ocean waves and above-freezing seawater. Under these conditions, the waves cut notches into the sides of the icebergs, where their penetration depths grow at speeds of meters-per-day. When the notch becomes deep enough, the overburden collapses, leaving an underwater foot, identical to that on which the Guardian collided and ran aground. The foot exerts a torque on the iceberg, which as the foot grows in length, fractures the iceberg. In support of this mechanism applying to the Guardian icebergs, the warm air temperatures between 10 and 15°C imply warm seawater, the collision is direct evidence of an underwater foot, and the iceberg sizes, with the possible exception of the one involved in the collision, were smaller than the scatterometer resolution.
When Wagner and others (Reference Wagner2014) apply their model to the BYU/NIC icebergs, they find that even as the iceberg size falls below the scatterometer resolution, the icebergs continue to drift as they shed smaller icebergs. Examination of their Figure 4c shows that two of BYU/NIC trajectories, when enhanced by the footloose model, continue to drift east in the ACC to the longitudes and approximate latitude of Riou's icebergs. This means that all the ship observations of icebergs are consistent with modern observations and theory.
5. Conclusions
This paper examines the distribution and properties of the icebergs observed during Cook's 1772–75 circumnavigation of Antarctica, Halley's 1700 traverse into the South Atlantic, Bouvet's 1739 discovery of Cape Circumcision and Riou's 1789 disastrous iceberg encounter in the Antarctic Circumpolar Current. Because the application of an ice drift and the footloose mechanism to the BYU/NIC trajectory data by England and others (Reference England, Wagner and Eisenman2020) explains the outliers observed by Riou, the distribution of all the ship-observed icebergs agrees with modern observations and theory. The largest iceberg Cook records had a 5 km2 area, and while Halley's largest iceberg had a 9 km waterline length, he provided no estimate of its area. Based on the power-law curve of Tournadre and others (Reference Tournadre, Bouhier, Girard-Ardhuin and Rémy2016), England and others (Reference England, Wagner and Eisenman2020) show that the size of Cook's largest iceberg is equal to or greater than at least 92% of the Antarctic icebergs. The fact that none of the ships observed giant icebergs is explained by their low probability of occurrence.
The areas of agreement between Cook's icebergs and modern data include their distribution in the Weddell Sea, the plume to the east of the Amery Ice Shelf and the results of his traverses in the Ross and Amundsen Seas. For sea ice, although Cook's sea-ice edge in regions other than the eastern Weddell Sea agrees with satellite observations, the large differences between his and satellite imagery of the sea-ice tongue remain unexplained (Parkinson, Reference Parkinson1990). Cook's transect onto the shelf of the ASE, where the ship attained its farthest south and Cook and Wales observed at least a hundred icebergs that probably calved from the Pine Island and Thwaites Glaciers, provides a remarkable precursor to the ITGC that began its fieldwork in 2018.
Supplementary material
The supplementary material for this article can be found at https://doi.org/10.1017/jog.2022.111
Data
The BYU/NIC data can be downloaded at www.scp.byu.edu/iceberg. Cook's and other shipboard iceberg positions are available in the Supplementary material. The AWI dataset is available from MPS at michael.p.schodlok@jpl.nasa.gov.
Acknowledgements
David G. Long's work was supported by the NASA Oceanography Program under Grant 80NSSC19K0057 and the NASA Cryospheric Science Program under Grant 80NSSC18K1055. Michael P. Schodlok's work was carried out at the Jet Propulsion Laboratory, California Institute of Technology, under a contract with the National Aeronautics and Space Administration. He gratefully acknowledges support from the NASA Cryospheric Science Program. S. M. thanks Rachel Clark, Claire Parkinson, Harry Stern and Till Wagner for comments, Jenny Uglow for her introduction to 18th century icebergs, Walt Meier for help with Figure 3 and the NSIDC, Doug MacAyeal for help with references related to the Amundsen Sea Embayment, and the University of Washington Libraries and Corey Murata for their help with publication costs. Finally, the authors thank Editor Hester Jiskoot and the unnamed reviewers for their comments, questions, and suggested revisions. These greatly improved the paper.
Author contributions
S. M. and D. G. L. conceived of the study, S. M. digitized the Cook iceberg data and wrote most of the manuscript, D. G. L. prepared Figure 2, M. P. S. worked on the AWI data. All authors contributed to the analysis of the results and to the writing of the manuscript. The authors declare they have no competing interests.
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