If colleagues at AWI discuss the pro and cons of both polar regions, Antarctica is the favorite in terms of the weather.
Although temperatures are low even during austral summer, quite often the sun shines for 24 hours. In a calm corner on deck, one can take a sunbath during spare time (Fig. 1). We enjoyed such conditions during our last visit (PS111) to this area 3 years ago. However, this year it is quite different. The weather is similar to the one in Fram Strait, the narrow sea between Svalbard and Greenland. The sun only shines sporadically, winds are often strong, and light snowfall hampers our regular helicopter operations. The onboard meteorologist, Steffen Schröter, explains why we face almost Arctic conditions down here in the Weddell Sea.
Those might be desperately disappointed, who have hoped for bright sunshine and high pressure during the COSMUS expedition. At the moment, the opposite dominates our weather. Above a coastal polynya in the eastern Weddell Sea, our main research area, patterns of bad weather often form. In addition, lined up like a pearl necklace, low pressure systems move regularly from Bransfield Strait to Droning Maud Land, bringing moist air from the South Atlantic and northern Weddell Sea towards the position of Polarstern (Fig. 2).
The warm, moist air mixes with cold air from the continent causing small low-pressure systems/troughs and, thus, low-altitude clouds together with snowfall (Fig. 3). Since the beginning of our cruise, the sky is grey – like in the Arctic. If high-pressure systems develop, they are weak and do not last long but lift the base of the clouds, supporting our helicopter operations. Momentarily, sunshine is rare, but the weather situation should change when sea ice formation closes the coastal polynya. As a consequence, cold and dry air dominates and high-pressure systems will form more frequently – we’ll see.
What is left are the answers to the questions of our last weekly report – did you answer everything correctly?
750 nautical miles of distance | How many kilometers? | 1390 km |
658 km of sea floor scanned | How many iceberg scars detected? | 167 |
14 square meters sampled | How many kilograms of sediment retrieved? | 1800 kg |
2 seals, 2578 dives | How many dive-meters in total? | 30793 m |
79819 liter sea water filtered | How many grams of microplastic? | Analysis only possible at home institute |
Mooring recovery: 6643 m of rope, 112 instruments | How many moorings recovered? | 11 moorings |
20 km distance, 6000 photos | How often did we see an octopus? | Octopus: 1000 times Sea cucumbers: 500 times |
27 profiles, 180 000 photos | How many GB of storage space? | 2.5 GB |
30.76 m ice cores, 6.4 km snow and sea-ice thickness transects | How many hours on the ice floe? | 21 h 35 min |
6 bio-ice cores | How many filters stored? | 270 |
Table 1: The answers to the questions of our previous weekly report. OFOBS: Ocean Floor Observation and Bathymetry System.
PS124 sends regards from the southwestern (76 °S 30 °W) Weddell Sea – discovered almost 100 years ago from the British Sailor James Weddell. Obviously due to favorable weather conditions, he sailed as far south as 74 °S, the northern position of some of our moorings.
Hartmut H. Hellmer (Chief Scientist)