Deutsches Ozeanographisches
Datenzentrum
Inventur der Polarstern-Reise PS138 (ArcWatch-1) (DOD-Ref-No.20230015)
Inventory of Polarstern Cruise PS138 (ArcWatch-1) (DOD-Ref-No.20230015)
| Plattform Platform |
Reise-Nr. Cruise-No. |
Zeitraum Period |
Projekt Project |
Arbeitsgebiet Working area |
|---|---|---|---|---|
| Polarstern | PS138 (ArcWatch-1) | 03.08.2023 - 30.09.2023 | Arctic Ocean Nansen Basin Amundsen Sea North Pole |
| Fahrtleiter Chief Scientist | Institut Institute | Auslaufhafen Port of departure | Einlaufhafen Port of return | Stationskarte Station map | Schiffsroute Trackchart |
|---|---|---|---|---|---|
| Boetius Antje | Alfred-Wegener-Institut fur Polar- und Meeresforschung | Troms? | Bremerhaven |
Ziel der Reise / Objectives of Cruise:
The rapid warming of the Arctic and sea ice retreat affect not only the hydrography of the Arctic Ocean, but also biogeochemical and biological processes in various ways. The expedition PS138 (ArcWatch-1) investigated the biology, chemistry and physics of sea ice, as well as the impact of sea ice retreat on the entire ocean system from the surface to the deep sea. Expedition PS138 started in Troms? on August 3, 2023.The route first took us north through Norwegian waters to the ice edge and to the first ice station at 84?N and 30?E. Our journey then continued east to 83?N 130?E, and from there to the North Pole, from where we headed south again at 60?E to the ice-edge and then to our home port of Bremerhaven. We studied the dynamics of first- and multiyear ice, as well as the role of summerly ice melt and re-growth in fall for the distribution of nutrients, productivity and the composition of pelagic and benthic communities, as well as the export of particulate matter to the deep sea. During the expedition PS80 (ARK27-3, IceArc) in 2012, which took place during the largest documented sea ice minimum to date, substantial impacts on the ecosystem were found. Eleven years later, the expedition PS138 has assessed the current ecosystem state and enabled comparative studies over the timeframe of several decades. We re-visited the same locations as in 2012, and used interdisciplinary process studies to examine interactions between ice physics and biology, hydrography, biogeochemistry and biodiversity of the Arctic ecosystem, from the sea ice to the seafloor. This included comparative studies between working areas in the marginal ice zone and areas covered by multiyear sea ice in the central Arctic Ocean. The work included the deployment of a range of established and novel technologies, for example moored lander systems and towed instruments. In addition to scientific operations on the sea ice and from board, short and long-term moorings were deployed to assess the physics, chemistry and biology of the Arctic Ocean across different temporal scales. In addition, we repeated some studies at former MOSAIC sites. The results from this expedition show several anomalies in 2023 and are an important contribution to quantifying the effects of changes in sea ice cover on the Arctic Ocean and its ecosystems.
Messungen / Measurements
| Institut Institute |
Wissenschaftler Scientist |
Anzahl Number |
Einheit Unit |
Typ der Messungen Type of measurements |
Kommentar Comments |
Daten im DOD Data in DOD |
|---|---|---|---|---|---|---|
| AWI | Eggers Sarah Lena | 10 | deployment | B08 Phytoplankton |
Hand Net. | no |
| AWI | Vane Kim | 9 | deployment | B09 Zooplankton |
The Bongo net that is towed obliquely for finding the larger-sized zooplankton, such as amphipods and krill. | no |
| AWI | Vane Kim | 18 | deployment | B09 Zooplankton |
Multinet. The Multinet which have fine mesh sizes for catching smaller organisms such as copepods. It samples vertically hauled. | no |
| AWI | Bienhold Christina | 20 | deployment | B16 Benthic bacteria / micro-organisms |
tv-guided multiple corer (12-core). This multi-corer is used to collect multiple undisturbed sediment samples including the sediment-water interface and overlying supernatant water, and sediment pore water at a high quality. In a tv-muc setup the multicorer is equipped with a video camera and telemetry to observe the seafloor, as well as instrument operation. | no |
| ISFWHV | Uhlir Carolin | 9 | deployment | B18 Zoobenthos |
Epibenthic Sledge (Brenke) DZMB | no |
| AWI | Bienhold Christina | 18 | deployment | B18 Zoobenthos |
Giant Box Corer. The Giant Box Corer samples a comparable large area of the sediment surface (50 x 50 cm) with minimal disturbance and collects a large block of sediment up to 60 cm below the sea floor. This gear is particularly useful for quantitative investigations of the benthic micro- to macrofauna. | no |
| AWI | Iversen Morten | 17 | deployment | B71 Particulate organic matter (e.g. POC, PON) |
Marine Snow Catcher | no |
| AWI | Bienhold Christina | 20 | deployment | B72 Biochemical measurements (e.g. lipids, aminoacids) |
tv-guided multiple corer (12-core). This multi-corer is used to collect multiple undisturbed sediment samples including the sediment-water interface and overlying supernatant water, and sediment pore water at a high quality. In a tv-muc setup the multicorer is equipped with a video camera and telemetry to observe the seafloor, as well as instrument operation. | no |
| AWI | Hoppmann Mario | 27 | deployment | D90 Other physical oceanographic measurements |
various buoy deployments | no |
| AWI | Purser Autun | 16 | deployment | G08 Bottom photography |
The vertically facing towed camera and acoustic system OFOBS (Ocean Floor Observation and Bathymetry System) is used to assess large-scale distribution patterns of larger epi-benthic organisms and other objects (e.g. dropstones, garbage) at the deep seafloor. The system is lowered to approx. 1.5 m above ground using a fibre optical cable for data, video and energy transfer, and then towed along a transect at a speed of 0.5 knots. | no |
| AWI | Wenzhofer Frank | 14 | deployment | G71 In-situ sea floor measurements |
Deep Sea Benthic Lander | no |
| FIELAX | Tardeck Frederic | 8 | profiles | G74 Multi-beam echosounding |
The Multibeam Echo Sounder uses several frequencies to map the topography of the seafloor. It also provides information about the texture of the seafloor as well as the structure of the water body. | no |
| AWI | Rabe Benjamin | 226 | stations | H00 Stations |
- | yes |
| AWI | Rabe Benjamin | 41 | deployment | H10 CTD-Stations |
The CTD probe measures conductivity and temperature along a vertical transect through the water body. The measured parameter are used to calculate the salinity of the water. Additionally, up to 24 water samples can be taken in different water depths during the CTD measurements. | no |
| AWI | Rabe Benjamin | 50 | deployment | H10 CTD-Stations |
eXpendable CTDs (XCTD) | no |
| AWI | Iversen Morten | 9 | deployment | R01 Water column photography |
Remotely Observing INsitu camera for Aggregates (ROSINA) | no |