LOGISTICS REPORT
K049 NZ ITASE – Holocene Climate Variability along the Victoria Land Coast
Antarctica New Zealand 2003/04
*AIMS
Seven key locations were identified for the NZ ITASE (International Transantarctic Scientific Expedition) programme. The analyses on the ice core from the first site, Victoria Lower Glacier in the McMurdo Dry Valleys, have almost been completed. For the 2003/04 field season we proposed to carry out a detailed reconnaissance and to recover intermediate length cores from sites 2 and 3: Evans Piedmont Glacier and Mt Erebus Saddle. Due to logistical constraints of Antarctica New Zealand the drilling was deferred to the 2004/05 season, but the reconnaissance was conducted.
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ITASE-Objective
The focus of the New Zealand ITASE group is to provide information from the climate sensitive, low altitude, coastal sites. This will capture the climate signature of the troposphere, which represents a regional account on the Ross Sea climate. The ice core data are expected to provide a record of air temperature, snow accumulation, precipitation source, atmospheric circulation strength, storm frequency, sea ice variation, ocean productivity, and anthropogenic influences. The results will help to decide whether the Ross Sea region is currently cooling or warming with a longer-term prospective, taking low frequency climate variability (100 to 1000 year cycles) into account. Furthermore, proposed tele-connections such as the Amundsen Low-ENSO correlation [Meyerson et al., 2002; Bertler et al., submitted] or the Southern Hemisphere Annual Mode [Thompson and Solomon, 2002] can be further constrained. -
Latitudinal Gradient Project Objective
The project is expected to contribute substantially to the Latitudinal Gradient Project, as it can provide a history of temperature, humidity, sea ice cover, precipitation source, atmospheric circulation, and ocean productivity along the Victoria Coast for the last 200 to 10,000 years. Furthermore, the timing and velocity of the Ross Ice Shelf retreat some 9 to 5ka years ago is still discussed controversially [Steig et al., 1998; Hall and Denton, 2000; Steig et al., 2000]. -
ANDRILL Objective
The ice core locations 2 and 3 (Evans Piedmont Glacier and Mt. Erebus Saddle) are in the vicinity of planned ANDRILL coring locations (Granite Harbour and Windless Bight). The ice core records will provide a high resolution climate dataset, which serves as a reference for the younger part of marine record recovered through ANDRILL. -
Longer-Term Mass Balance Objective
During the 1999/2000 season mass balance measurement devices (submerge velocity method [Hamilton et al., 1998; Hamilton and Whillans, 2000]) have been deployed at Victoria Lower Glacier. The device has since been revisited during season 2000/2001 and 2001/2002. The measurements show that the glacier has a slightly negative mass balance, losing around 12cm thickness per year. A continuation of the measurements will allow monitoring changes in the ablation intensity of the McMurdo Dry Valleys. -
The Antarctic – New Zealand Connection Objective
New Zealand's future economic and social development, environmental sustainability, and infrastructural planning relies critically upon the accurate assessment of the impact of "global warming" in our sector of the planet. Future climate change is a result of both natural variability and anthropogenic influence. A joint programme between IGNS, University of Maine, Victoria page 2 University is investigating ice core records from New Zealand (Tasman Glacier and Mt. Ruapehu ice field). The comparison between our NZ and Antarctic ice core records will provide much needed data for the development of realistic regional climate models to predict NZ climate in the 21th Century [Mullan et al., 2001].
*PERSONNEL
Name | Designation | Organisation | Departed Chch | Returned Chch |
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Nancy Bertler | PI | Antarctic Research Centre, Victoria Uni | 7 Nov | 8 Dec |
Alex Pyne | Drilling Specialist | Antarctic Research Centre, Victoria Uni | 7 Nov | 6 Dec |
Matt Watson | GPR Specialist | Scan Tec | 12 Nov | 6 Dec |
Louise Christie | Student Assistant | School of Earth Sciences, Victoria Uni | 7 Nov | 6 Dec |
Matt Wood | Student Assistant | School of Earth Sciences, Victoria Uni | 7 Nov | 6 Dec |
Ewan Patterson | Glacier Travel Specialist | Antarctica New Zealand | NA | NA |
*PLANNING
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Application process
The application process was organised in professional and efficient manner. However, it would be of advantage if the NZ review of a science proposal was transferred to an overseas reviewer if there is no NZ expert can be found. The assessment of the value of the proposed science from a non-expert is likely to be misleading. -
Communications with Antarctica New Zealand staff
Antarctica New Zealand staff appears very competent and helpful. The planning for this event required significant time and resources and logistic re-evaluation, especially when Antarctica New Zealand logistic constraints limited this seasons programme to site survey only. It was an understanding that Antarctica New Zealand agreed that the drilling component would be supported the following season. -
Provision of maps and aerial photographs
N.A. -
Pre-season information
The information received was timely and valuable -
Medicals, documentation and flights to Antarctica
The information received was timely and valuable
*PREPARATIONS FOR THE FIELD
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Reception and planning for your event
The reception was well organised, friendly and efficient. The main issues of the event were promptly discussed and organisedpage 3 -
Availability and condition of equipment received
The equipment requested from Scott Base was supplied in time and in good condition. This included two skidoos, one nansen sledge, two generator and field equipment including a polar haven tent. -
Field training
The field training was helpful and appropriate for the new members of our team. The full AFT training for Pyne and Bertler was unhelpful and a waste of resources and time. The additional crevasse rescue training was appreciated and very efficient. The frequency of full AFT requirements for experienced people should be reviewed to take account of personal experience and regular Antarctic activity that includes fieldwork. The "current" 3 year frequency is too short. -
Field party equipment 'shakedown' journey
N.A. -
Delays at Scott Base, whatever the cause
All staff at Scott Base were very helpful and supportive, allowing a smooth operation of our project. The only reason for prolonged delay at Scott Base was bad weather conditions postponing helicopter moves. -
Safety and Risk Management processes
The safety and risk management appears sound and efficient -
General comments about Scott Base
The staff at Scott Base create a very friendly, supportive environment. We are grateful for the helpful and professional support we received from Scott Base staff.
FIELD TRANSPORT
Fig.3: GPR/GPS set-up. A 400MHz antenna travels in front of the first skidoo. A second skidoo tails the set-up for crevasse safety.
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Vehicles
The two allocated skidoos (Alpine II) were in good condition and performed well. However, our GPR traverses on the Evans Piedmont Glacier were reduced due to rough surface conditions, which proved too demanding on the skidoos and the technical equipment mounted on the Nansen sledge. The skidoos and Nansen were used primarily for GPR survey in a crevasse travel configuration. This is a relatively light weight operation and could be improved with lighter vehicles and sledge, especially when vehicles are flown to site. The GPR setup on the sledge could also be improved if a suitable sledge was pre-dedicated.page 4 - Aircraft Operations
- All our helicopter moves were done by HNO. We enjoyed the professionalism, friendliness and efficiency of the HNO staff, Rob McPhail and Richard Desborough. Difficult cargo such as skidoos, nansen sledge and fuel barrels was handled in a very professional and safe manner. None of our loads got damaged or lost although the underslung Nansen sledge was a slow load to fly.
Date | Location | PAX | Total Weight (lbs) |
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11 Nov | SB to CR | 4 | 1830 |
11 Nov | CR to VLG (failed due to lack of surface definition) - unload at MP | 3 | 1800 |
12 Nov | MP to VLG | 3 | 1800 |
12 Nov | CP to VLG (pick up of traversed equipment) | 0 | 800 |
14 Nov | VLG to EPG (via CR) | 4 | 2800 |
15 Nov | SB to EPG | 2 | 3200 |
21 Nov | EPG to CR (Pyne and Wood transfer to K042) | 2 | 1000 |
25 Nov | EPG to SB | 4 | 5100 |
4 Dec | SB to MES to SB (reconnaissance) | 4 | 1200 |
*EVENT DIARY
Date | Main Activities and Location | Other Comments |
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07 Nov | Arrival at Scott Base | |
08 Nov | AFT training for all K049 members | |
09 Nov | AFT training for all K049 members | |
10 Nov | Equipment shake-down and field preparation | |
11 Nov | First attempt to put-in to first site, Victoria Lower Glacier. Lack of surface definition prohibited landing and Bertler, Christie, and Wood are dropped at Marble Point. Pyne was moved to Cape Roberts for work on the tide gauge (K042) | |
12 Nov | Put-in to Victoria Lower Glacier, camp set-up, deployment of base station at 3km distant Staeffler Ridge, commencement of first mass balance measurement | |
13 Nov | Continuation of mass balance survey at 4km distant Victoria Lower Glacier II site | |
14 Nov | Bertler, Pyne, Christie, and Wood move camp to Evans Piedmont Glacier after site reconnaissance. Camp set-up, deployment of GPS base station | |
15 Nov | Watson and Paterson arrive at Evans Piedmont. Set-up of traverse equipment (ground penetrating radar and GPS) on Nansen sledge. Set-up of traverse line (skidoo-sledge-skidoo). Preparation for snow pit work. | |
16 Nov | Excavation of 4m deep snow pit. Assemblage of GPR and GPS equipment . | |
17 Nov | Bertler, Watson, Paterson, Wood start GPR traverse; page 5 Pyne and Christie commence snow density and temperature measurement in the snow pit. | |
18 Nov | Bertler, Watson, Paterson, Wood continue GPR traverse; Pyne and Christie continue snow density and temperature measurement in the snow pit. | |
19 Nov | Pyne, Watson, Paterson, Christie continue GPR traverse; Wood continue snow density and temperature measurement in the snow pit, Bertler commences snow sampling in the snow pit. | Due to bad weather conditions all activities were aborted at lunch time. |
20 Nov | Confined to tents, hourly sampling of snow precipitation | Due to bad weather conditions all activities were aborted |
21 Nov | Pyne and Wood move to Cape Roberts (K042). Bertler, Watson, Paterson, and Christie continue GPR traverse. Bertler and Christie continue snow pit work | Visit by NZ Herold and Lou Sanson |
22 Nov | Bertler, Watson, Paterson, and Christie continue GPR traverse. Bertler and Christie continue snow pit work | Radio interview with NZ Harold, Simon Collins |
23 Nov | Bertler, Watson, Paterson, and Christie continue GPR traverse. Bertler and Christie continue snow pit work | |
24 Nov | Bertler, Watson, Paterson, and Christie continue GPR traverse. Bertler and Christie continue snow pit work | |
25 Nov | Bertler, Watson, Paterson, and Christie move to Scott Base. | |
26 Nov to 3 Dec | Scheduled reconnaissance for Mt Erebus Saddle is deferred due to bad weather. GPR, GPS, and density data processing at Scott Base. | |
4 Dec | Bertler, Pyne, Watson, and Paterson conduct 5 hour reconnaissance at Mt Erebus Col and Mt Terra Nova | |
6 Dec | Pyne, Watson, Wood, and Christie return to NZ | |
8 Dec | Bertler returns to NZ |
*WEATHER
In total we lost 12 days of fieldwork due to bad weather conditions, which amounts to 43% of our time in Antarctica. However, due to the commitment of each member of K049 and the exceptional support by Scott Base and HNO staff we were able to conduct most of what was proposed nonetheless. We encountered two snow storms while based at Evans Piedmont Glacier, which provided us with the possibility to hourly snow sampling for airmass trajectory reconstruction. The longest delay due to weather conditions for us occurred when we tried to put in to Mt Erebus Saddle for 8 days, which caused the early termination of our season this year. However, a 5hour weather clearance allowed us a reconnaissance in which we gathered the necessary information to conduct the drilling at this site during 2004/05.
*ACCIDENTS, INCIDENTS OR HAZARDS
None of the above occurred or were observed
FIELD EQUIPMENT
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Quality, suitability and performance of field clothing
The issued field clothing was appropriate and functional. -
Performance and design of tents, technical climbing equipment, kitchen gear and sledges
The supplied field equipment was in good condition and very reliable. We are especially grateful for the allocation of the polar haven tent, as it allowed us to maintain and repair our electronic and computer equipment. The polar haven tent was set up with a VUW sigma heater and a LPG gas cooker. The crevasse safety and rescue equipment was in good condition and efficient. -
20 person day ration box system
The food boxes were well packed in terms of quantity and nutrition. The provision of bulk food supply for medium sized field parties still has scope for improvement and development.
RADIO COMMUNICATIONS
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Suitability and effectiveness of the radio equipment
The radio equipment was in excellent condition and we appreciated the professional advice by Keith Roberts -
Reception/transmission conditions and suitability of radio schedule timing
Reception and transmission were generally good and the timing of the radio schedule convenient -
Scott Base's general efficiency during radio schedule
Radio communication was mainly very efficient, professional and appreciated
COMPUTER FACILITIES
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Suitability and effectiveness of computer network
The computer network met our needs satisfactorily. A possibility to connect laptops to the Scott Base external net connection would be highly appreciated, especially during prolonged delays at Scott Base. -
Quality, suitability and performance of public computers
The quality and suitability of public computers was sufficient and appreciated, albeit somewhat busy.
*ENVIRONMENTAL IMPACT
*Sites Visited
Site name | Victoria Lower Glacier |
Site location (coordinates/description) | 77°43.7S, 162°33.7E, glacier surface |
Dates occupied | 12 Nov 2003 – 14 Nov 2003 |
Total days (or hours) at site | 3 days |
Maximum number of people at site | 3 |
Total person-days (or person-hours) at site | 9 |
Main activity undertaken | Mass balance measurement |
Equipment installed/left in field
Type of equipment/marker installed | Submergence velocity device for mass balance measurement (Fig.2) |
Location of installation left in field | VLG Ia 77°19′48.3245S, 162°31′55.5141E VLG Ib 77°19′48.3243S, 162°31′55.4501E VLG II 77°20′49.1079S, 162°29′32.2241E |
Size of items left in field | 3m stainless tube, 0.4×0.4m plywood |
Number of items left in field | 3 |
Date of intended retrieval | End of project |
*Other environmental impacts
None
*Differences from original Preliminary Environmental Evaluation (PEE)
None
*Sites Visited
Site name | Evans Piedmont Glacier |
Site location (coordinates/description) | 77°43.7S, 162°33.7E, glacier surface |
Dates occupied | 14 Nov 2003 to 25 Nov 2003 |
Total days (or hours) at site | 12 days |
Maximum number of people at site | 6 |
Total person-days (or person-hours) at site | 60 |
Main activity undertaken | Ground penetrating radar survey and snow properties analysis |
Geological Material
Location | 77°43.7S, 162°33.7E |
Specimen type | Snow samples |
Quantity (kg) | 20 kg |
*Other environmental impacts
Exhaust fumes and noise from skidoos and generators used to conduct the site survey
*Differences from original Preliminary Environmental Evaluation (PEE)
None
*Sites Visited
Site name | Mt Erebus Saddle and Mt Terra Nova |
Site location (coordinates/description) | 77° 30.832S, 167°40.216 and 77°31.375S, 167°55.864E |
Dates occupied | 04 Dec 2003 |
Total days (or hours) at site | 5 hours (total) |
Maximum number of people at site | 5 |
Total person-days (or person-hours) at site | 25 person-hours |
Main activity undertaken | Ground penetrating radar survey and snow properties analysis |
*Other environmental impacts
None
*Differences from original Preliminary Environmental Evaluation (PEE)
None