Ground- and ship-based microwave radiometer measurements during EUREC4A

• Published in: Earth System Science Data
• Main Authors: Schnitt, Sabrina, Foth, Andreas, Kalesse-Los, Heike, Mech, Mario, Acquistapace, Claudia, Jansen, Friedhelm, Löhnert, Ulrich, Pospichal, Bernhard, Röttenbacher, Johannes, Crewell, Susanne, Stevens, Bjorn
• Format: Text
• Language: English
• Published: 2024
• Subjects: North Atlantic
• Online Access: https://doi.org/10.5194/essd-16-681-2024; https://essd.copernicus.org/articles/16/681/2024/

During the EUREC 4 A field study, microwave radiometric measurements were performed at Barbados Cloud Observatory (BCO) and aboard RV Meteor and RV Maria S Merian in the downstream winter trades of the North Atlantic. We present retrieved integrated water vapor (IWV), liquid water path (LWP), and temperature and humidity profiles as a unified, quality-controlled, multi-site data set on a 3 s temporal resolution for a core period between 19 January and 14 February 2020 in which all instruments were operational. Multi-channel radiometric measurements were performed at BCO and aboard RV Meteor between 22 and 31 GHz (K-band) and from 51 to 58 GHz (V-band). Combined radar–radiometer measurements of a W-band Doppler radar with a single-channel radiometer instrument were conducted at 89 GHz aboard RV Meteor and RV Maria S Merian . We present a novel retrieval method to retrieve LWP from single-channel 89 GHz measurements, evaluate retrieved quantities with independent measurements, and analyze retrieval uncertainties by site and instrument intercomparison. Mean IWV conditions of 31.8 kg m −2 match independent radiosoundings at BCO with a root-mean-square difference of 1.1 kg m −2 . Mean LWP conditions in confidently liquid cloudy, non-precipitating conditions ranged between 63.1 g m −2 at BCO and 46.8 g m −2 aboard RV Maria S Merian . Aboard the ships, 90 % of LWP was below 120 g m −2 with a 30 % uncertainty for LWP of 50 g m −2 . Up to 20 % of confidently liquid cloudy profiles ranged below the LWP detection limit due to optically thin clouds. The data set comprises of processed raw data (Level 1), full quality-controlled post-processed instrument data (Level 2), a unified temporal resolution (Level 3), and a ready-to-use multi-site time series of IWV and LWP (Level 4), available to the public via AERIS ( https://doi.org/10.25326/454##v2.0 Schnitt et al. , 2023 a ). The data set complements the airborne LWP measurements conducted during EUREC 4 A and provides a unique benchmark tool for satellite evaluation and ...