-
Continuous measurements in soil and air at the permafrost long-term observato...
Understanding permafrost processes and changes requires long-term observational datasets. This dataset is a continuation of the dataset available from the long-term... -
Calm data at station Samoylov (2024)
Understanding permafrost processes and changes requires long-term observational datasets. This dataset is a continuation of the dataset available from the long-term... -
Meteorological and soil data from Bayelva, Svalbard, homogenised data product...
Understanding permafrost processes and their links to polar climate requires long-term observational datasets. This data product is a quality-controlled and homogenised... -
Meteorological and soil data from Bayelva, Svalbard, homogenised data product...
Understanding permafrost processes and their links to polar climate requires long-term observational datasets. This data product is a quality-controlled and homogenised... -
Soil data at station Bayelva (2023, level 1)
Understanding permafrost processes and changes requires long-term observational datasets. This dataset is a continuation of the dataset available from the Bayelva Site at... -
Soil data at station Bayelva (2022, level 1)
Understanding permafrost processes and changes requires long-term observational datasets. This dataset is a continuation of the dataset available from the Bayelva Site at... -
Soil data at station Bayelva (2021, level 1)
Understanding permafrost processes and changes requires long-term observational datasets. This dataset is a continuation of the dataset available from the Bayelva Site at... -
Soil data at station Bayelva (2020, level 1)
Understanding permafrost processes and changes requires long-term observational datasets. This dataset is a continuation of the dataset available from the Bayelva Site at... -
Soil data at station Bayelva (2019, level 1)
Understanding permafrost processes and changes requires long-term observational datasets. This dataset is a continuation of the dataset available from the Bayelva Site at... -
Soil data at station Bayelva (2018, level 1)
This dataset has no description
-
Aerobic carbon dioxide production data of permafrost-affected soils of the no...
We aerobically incubated soil samples from a polygon center (P3, 72° 22.5 N, 126° 29.4 E) on Samoylov, Northeast Siberia for 150 days. We used three soil layers ((i) surface... -
Aerobic carbon dioxide production data of permafrost-affected soils of the no...
We aerobically incubated soil samples from a polygon center (P3, 72° 22.5 N, 126° 29.4 E) on Samoylov, Northeast Siberia for 150 days. We used three soil layers ((i) surface... -
Anaerobic carbon dioxide and methane production data of control and freeze-th...
We anaerobically incubated soil samples from a polygon center (P2, 72° 22.3 N, 126° 29.9 E) on Samoylov, Northeast Siberia at 4°C for 60 days. We used three soil layers ((i)... -
Aerobic carbon dioxide production data of control and freeze-thaw permafrost-...
We aerobically incubated soil samples from a polygon center (P1, 72° 22.5 N, 126° 29.4 E) on Samoylov, Northeast Siberia at 4°C for 60 days. We used three soil layers ((i)... -
Anaerobic carbon dioxide and methane production data of permafrost-affected s...
We anaerobically incubated soil samples from two polygon centers (P1: 72° 22.5 N, 126° 29.4 E, P2: 72° 22.3 N, 126° 29.9 E) on Samoylov, Northeast Siberia at 4°C for 150 days.... -
Aerobic carbon dioxide production data of permafrost-affected soils of the no...
Soil and incubation data of permafrost-affected soils of the northeast Siberian polygonal tundra -
Temperature measurements at Brandallaguna in March 2021
Bottom water temperatures in lakes and the near-shore Arctic Ocean are usually below 4°C. If the water depth is shallow enough, the sea/lake ice freezes to the sea/lake bed and... -
Meteorological and soil data from Bayelva, Svalbard, homogenised data product...
Understanding permafrost processes and their links to polar climate requires long-term observational datasets. This data product is a quality-controlled and homogenised... -
Continuous measurements in soil and air at the permafrost long-term observato...
Understanding permafrost processes and changes requires long-term observational datasets of ground and climate variables. Despite the fact that the Arctic climate changes more... -
Soil and incubation data of permafrost-affected soils of the northeast Siberi...
The large amounts of soil organic matter (SOM) in permafrost-affected soils are prone to increased microbial decomposition in a warming climate. The environmental parameters...
