cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.857098
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/1 at station 2290

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.857100
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/1 at station 028

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.857102
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/1 at station 048

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.857116
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/2 at station M103/2_081

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.857117
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/2 at station M103/2_083

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.857118
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/2 at station M103/2_088

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.857119
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/2 at station M103/2_089

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.857120
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/2 at station M103/2_104

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.857121
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/2 at station M103/2_107

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.857122
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/2 at station M103/2_110

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.857123
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/2 at station M103/2_114

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.857124
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/2 at station M103/2_118

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.857125
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/2 at station M103/2_119

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.857126
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/2 at station M103/2_120

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.857127
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/2 at station M103/2_121

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.857128
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/2 at station M103/2_123

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.857129
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/2 at station M103/2_127

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.857130
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/2 at station M103/2_131

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.857131
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/2 at station M103/2_135

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.857132
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/2 at station M103/2_144

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.857133
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/2 at station M103/2_147

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.857134
title: Incident irradiance above water and upward radiance below the water surface during METEOR cruise M103/2 at station M103/2_148

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.857218
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/2 at station 081

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.857220
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/2 at station 083

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.857221
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/2 at station 088

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.857222
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/2 at station 089

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.857223
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/2 at station 104

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.857224
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/2 at station 107

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.857225
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/2 at station 110

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.857226
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/2 at station 114

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.857227
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/2 at station 118

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.857228
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/2 at station 119

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.857229
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/2 at station 120

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.857230
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/2 at station 121

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.857231
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/2 at station 123

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.857232
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/2 at station 127

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.857233
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/2 at station 131

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.857234
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/2 at station 135

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.857235
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/2 at station 144

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.857236
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/2 at station 147

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.857237
title: Profiles of downward irradiance and upward radiance during METEOR cruise M103/2 at station 148

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.859049
title: Physical oceanography from CTD measured during METEOR expedition M103/1
DOI: 10.1594/pangaea.859050
title: Physical oceanography from CTD measured during METEOR expedition M103/2
DOI: 10.1594/pangaea.859209
title: 1) δ¹³C-CO2 and d15N-N2 isotope ratios in EDC, EDML and Talos Dome ice cores measured by sublimation extraction
DOI: 10.1594/pangaea.859600
title: Basic measurements of radiation at station Lindenberg (2007-06)
DOI: 10.1594/pangaea.859605
title: Basic measurements of radiation at station Lindenberg (2007-07)
DOI: 10.1594/pangaea.859623
title: Basic measurements of radiation at station Lindenberg (2007-08)
DOI: 10.1594/pangaea.859629
title: Basic measurements of radiation at station Lindenberg (2007-09)
DOI: 10.1594/pangaea.859634
title: Basic measurements of radiation at station Lindenberg (2007-10)
DOI: 10.1594/pangaea.859652
title: Basic measurements of radiation at station Lindenberg (2007-05)
DOI: 10.1594/pangaea.871624
title: Basic measurements of radiation at station Lindenberg (2009-01)
DOI: 10.1594/pangaea.869220
title: Basic measurements of radiation at station Lindenberg (2008-03)
DOI: 10.1594/pangaea.869227
title: Basic measurements of radiation at station Lindenberg (2008-04)
DOI: 10.1594/pangaea.869235
title: Basic measurements of radiation at station Lindenberg (2008-05)
DOI: 10.1594/pangaea.869249
title: Basic measurements of radiation at station Lindenberg (2008-06)
DOI: 10.1594/pangaea.869254
title: Basic measurements of radiation at station Lindenberg (2008-07)
DOI: 10.1594/pangaea.869261
title: Basic measurements of radiation at station Lindenberg (2008-08)