cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.856943
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/1 at station 002

description: The incident irradiance above water Es (lambda) and the upward radiance just below the water surface Lu (lambda,0-) were measured with Satlantic surface reference (SMSR-SeaWiFS Multichannel Surface Reference) in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.856944
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/1 at station 006

description: The incident irradiance above water Es (lambda) and the upward radiance just below the water surface Lu (lambda,0-) were measured with Satlantic surface reference (SMSR-SeaWiFS Multichannel Surface Reference) in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.856945
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/1 at station 007

description: The incident irradiance above water Es (lambda) and the upward radiance just below the water surface Lu (lambda,0-) were measured with Satlantic surface reference (SMSR-SeaWiFS Multichannel Surface Reference) in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.856946
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/1 at station 009

description: The incident irradiance above water Es (lambda) and the upward radiance just below the water surface Lu (lambda,0-) were measured with Satlantic surface reference (SMSR-SeaWiFS Multichannel Surface Reference) in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.856947
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/1 at station 010

description: The incident irradiance above water Es (lambda) and the upward radiance just below the water surface Lu (lambda,0-) were measured with Satlantic surface reference (SMSR-SeaWiFS Multichannel Surface Reference) in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.856948
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/1 at station 018

description: The incident irradiance above water Es (lambda) and the upward radiance just below the water surface Lu (lambda,0-) were measured with Satlantic surface reference (SMSR-SeaWiFS Multichannel Surface Reference) in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.856949
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/1 at station 020

description: The incident irradiance above water Es (lambda) and the upward radiance just below the water surface Lu (lambda,0-) were measured with Satlantic surface reference (SMSR-SeaWiFS Multichannel Surface Reference) in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.856950
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/1 at station 028

description: The incident irradiance above water Es (lambda) and the upward radiance just below the water surface Lu (lambda,0-) were measured with Satlantic surface reference (SMSR-SeaWiFS Multichannel Surface Reference) in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.856951
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/1 at station 035

description: The incident irradiance above water Es (lambda) and the upward radiance just below the water surface Lu (lambda,0-) were measured with Satlantic surface reference (SMSR-SeaWiFS Multichannel Surface Reference) in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.856952
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/1 at station 038

description: The incident irradiance above water Es (lambda) and the upward radiance just below the water surface Lu (lambda,0-) were measured with Satlantic surface reference (SMSR-SeaWiFS Multichannel Surface Reference) in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.856953
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/1 at station 042

description: The incident irradiance above water Es (lambda) and the upward radiance just below the water surface Lu (lambda,0-) were measured with Satlantic surface reference (SMSR-SeaWiFS Multichannel Surface Reference) in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.856954
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/1 at station 043

description: The incident irradiance above water Es (lambda) and the upward radiance just below the water surface Lu (lambda,0-) were measured with Satlantic surface reference (SMSR-SeaWiFS Multichannel Surface Reference) in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.856955
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/1 at station 046

description: The incident irradiance above water Es (lambda) and the upward radiance just below the water surface Lu (lambda,0-) were measured with Satlantic surface reference (SMSR-SeaWiFS Multichannel Surface Reference) in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.856956
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/1 at station 048

description: The incident irradiance above water Es (lambda) and the upward radiance just below the water surface Lu (lambda,0-) were measured with Satlantic surface reference (SMSR-SeaWiFS Multichannel Surface Reference) in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.856957
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/1 at station 049

description: The incident irradiance above water Es (lambda) and the upward radiance just below the water surface Lu (lambda,0-) were measured with Satlantic surface reference (SMSR-SeaWiFS Multichannel Surface Reference) in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.856958
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/1 at station 057

description: The incident irradiance above water Es (lambda) and the upward radiance just below the water surface Lu (lambda,0-) were measured with Satlantic surface reference (SMSR-SeaWiFS Multichannel Surface Reference) in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.856959
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/1 at station 061

description: The incident irradiance above water Es (lambda) and the upward radiance just below the water surface Lu (lambda,0-) were measured with Satlantic surface reference (SMSR-SeaWiFS Multichannel Surface Reference) in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.856960
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/1 at station 2281

description: The incident irradiance above water Es (lambda) and the upward radiance just below the water surface Lu (lambda,0-) were measured with Satlantic surface reference (SMSR-SeaWiFS Multichannel Surface Reference) in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.856961
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/1 at station 2282

description: The incident irradiance above water Es (lambda) and the upward radiance just below the water surface Lu (lambda,0-) were measured with Satlantic surface reference (SMSR-SeaWiFS Multichannel Surface Reference) in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.856962
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/1 at station 2286

description: The incident irradiance above water Es (lambda) and the upward radiance just below the water surface Lu (lambda,0-) were measured with Satlantic surface reference (SMSR-SeaWiFS Multichannel Surface Reference) in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.856963
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/1 at station 2287

description: The incident irradiance above water Es (lambda) and the upward radiance just below the water surface Lu (lambda,0-) were measured with Satlantic surface reference (SMSR-SeaWiFS Multichannel Surface Reference) in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.856964
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/1 at station 2289

description: The incident irradiance above water Es (lambda) and the upward radiance just below the water surface Lu (lambda,0-) were measured with Satlantic surface reference (SMSR-SeaWiFS Multichannel Surface Reference) in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.856965
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/1 at station 2290

description: The incident irradiance above water Es (lambda) and the upward radiance just below the water surface Lu (lambda,0-) were measured with Satlantic surface reference (SMSR-SeaWiFS Multichannel Surface Reference) in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.857072
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/1 at station 001

description: Vertical profiles of downward irradiance Ed (z,lambda) and upward radiance Lu (z,lambda) were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.857073
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/1 at station 002

description: Vertical profiles of downward irradiance Ed (z,lambda) and upward radiance Lu (z,lambda) were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.857074
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/1 at station 006

description: Vertical profiles of downward irradiance Ed (z,lambda) and upward radiance Lu (z,lambda) were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.857075
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/1 at station 007

description: Vertical profiles of downward irradiance Ed (z,lambda) and upward radiance Lu (z,lambda) were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.857076
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/1 at station 009

description: Vertical profiles of downward irradiance Ed (z,lambda) and upward radiance Lu (z,lambda) were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.857077
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/1 at station 010

description: Vertical profiles of downward irradiance Ed (z,lambda) and upward radiance Lu (z,lambda) were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.857078
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/1 at station 018

description: Vertical profiles of downward irradiance Ed (z,lambda) and upward radiance Lu (z,lambda) were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.857079
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/1 at station 020

description: Vertical profiles of downward irradiance Ed (z,lambda) and upward radiance Lu (z,lambda) were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.857084
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/1 at station 035

description: Vertical profiles of downward irradiance Ed (z,lambda) and upward radiance Lu (z,lambda) were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.857085
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/1 at station 038

description: Vertical profiles of downward irradiance Ed (z,lambda) and upward radiance Lu (z,lambda) were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.857086
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/1 at station 042

description: Vertical profiles of downward irradiance Ed (z,lambda) and upward radiance Lu (z,lambda) were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.857087
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/1 at station 043

description: Vertical profiles of downward irradiance Ed (z,lambda) and upward radiance Lu (z,lambda) were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.857088
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/1 at station 046

description: Vertical profiles of downward irradiance Ed (z,lambda) and upward radiance Lu (z,lambda) were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.857090
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/1 at station 049

description: Vertical profiles of downward irradiance Ed (z,lambda) and upward radiance Lu (z,lambda) were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.857091
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/1 at station 057

description: Vertical profiles of downward irradiance Ed (z,lambda) and upward radiance Lu (z,lambda) were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.857092
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/1 at station 061

description: Vertical profiles of downward irradiance Ed (z,lambda) and upward radiance Lu (z,lambda) were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.857093
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/1 at station 2281

description: Vertical profiles of downward irradiance Ed (z,lambda) and upward radiance Lu (z,lambda) were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.857094
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/1 at station 2282

description: Vertical profiles of downward irradiance Ed (z,lambda) and upward radiance Lu (z,lambda) were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.857095
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/1 at station 2286

description: Vertical profiles of downward irradiance Ed (z,lambda) and upward radiance Lu (z,lambda) were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.857096
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/1 at station 2287

description: Vertical profiles of downward irradiance Ed (z,lambda) and upward radiance Lu (z,lambda) were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.857097
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/1 at station 2289

description: Vertical profiles of downward irradiance Ed (z,lambda) and upward radiance Lu (z,lambda) were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.