Water vapour mixing ratio over Ny-Alesund from LiDAR measurements 2015-2018

Using the Raman channels of the Koldeway Aerosol Raman Lidar (KARL) a water vapour mixing ratio is derived. Data is availiable for all measurements during the dark season since 2015. Calibration in the winters 2015/2016 and 2016/2017 was performed using the GRUAN radiosounding product. For compariso...

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Bibliographic Details
Main Authors: Kulla, Birte Solveig, Ritter, Christoph
Format: Dataset
Language:English
Published: PANGAEA 2018
Subjects:
AC3
Arctic Amplification
Atmospheric Physics @ AWI
AWI_AtmoPhy
Monitoring station
MONS
NYA
Ny-Ålesund
Spitsbergen
Arctic
Ny Ålesund
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.896486
https://doi.org/10.1594/PANGAEA.896486
Description
Summary:Using the Raman channels of the Koldeway Aerosol Raman Lidar (KARL) a water vapour mixing ratio is derived. Data is availiable for all measurements during the dark season since 2015. Calibration in the winters 2015/2016 and 2016/2017 was performed using the GRUAN radiosounding product. For comparison those winters where recalculated with radiosounding measurements processed by the Vaisala Algorithm. The winter 2017/2018 is calibrated using radiosounding measurement from the RS41processed by the Vaisala Algrithm. The details of the calibration of this water vapour product are explained in Kulla & Ritter 2019.

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