77 datasets found

A radiation station was installed on drifting sea-ice in the Arctic Ocean during the MOSAiC expedition between November 2019 and September 2020. The station measured all the...

Understanding permafrost processes and changes requires long-term observational datasets of ground and climate variables. Despite the fact that the Arctic climate changes more...

Understanding permafrost processes and changes requires long-term observational datasets. This dataset is a continuation of the dataset available from the Bayelva Site at...

Understanding permafrost processes and changes requires long-term observational datasets. This dataset is a continuation of the dataset available from the Bayelva Site at...

Understanding permafrost processes and changes requires long-term observational datasets. This dataset is a continuation of the dataset available from the Bayelva Site at...

Understanding permafrost processes and changes requires long-term observational datasets. This dataset is a continuation of the dataset available from the Bayelva Site at...

Understanding permafrost processes and changes requires long-term observational datasets. This dataset is a continuation of the dataset available from the Bayelva Site at...

Understanding permafrost processes and changes requires long-term observational datasets. This dataset is a continuation of the dataset available from the Bayelva Site at...

The tethered balloon system BELUGA (Balloon-bornE moduLar Utility for profilinG the lower Atmosphere) was operated from an ice floe next to IB ODEN (around 89°37.0' N ,...

In a new version of the data (see doi:10.1594/PANGAEA.933223), the wind speed calibration for the standard meteorology sonde has been revised. Therefore please use the new version.

In a new version of the data (see doi:10.1594/PANGAEA.933223), the wind speed calibration for the standard meteorology sonde has been revised. Therefore please use the new version.

In a new version of the data (see doi:10.1594/PANGAEA.933223), the wind speed calibration for the standard meteorology sonde has been revised. Therefore please use the new version.

In a new version of the data (see doi:10.1594/PANGAEA.933223), the wind speed calibration for the standard meteorology sonde has been revised. Therefore please use the new version.

In a new version of the data (see doi:10.1594/PANGAEA.933223), the wind speed calibration for the standard meteorology sonde has been revised. Therefore please use the new version.

In a new version of the data (see doi:10.1594/PANGAEA.933223), the wind speed calibration for the standard meteorology sonde has been revised. Therefore please use the new version.

In a new version of the data (see doi:10.1594/PANGAEA.933223), the wind speed calibration for the standard meteorology sonde has been revised. Therefore please use the new version.

In a new version of the data (see doi:10.1594/PANGAEA.933223), the wind speed calibration for the standard meteorology sonde has been revised. Therefore please use the new version.

In a new version of the data (see doi:10.1594/PANGAEA.933223), the wind speed calibration for the standard meteorology sonde has been revised. Therefore please use the new version.

In a new version of the data (see doi:10.1594/PANGAEA.933223), the wind speed calibration for the standard meteorology sonde has been revised. Therefore please use the new version.

In a new version of the data (see doi:10.1594/PANGAEA.933223), the wind speed calibration for the standard meteorology sonde has been revised. Therefore please use the new version.