cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.966779
title: Continuous meteorological observations at DynaCom automatic weather station, Spiekeroog, Germany, 2023-10

description: Data presented here were collected between January 2022 to December 2023 within the research unit DynaCom (Spatial community ecology in highly dynamic landscapes: From island biogeography to metaecosystems, https://uol.de/dynacom/ ) of the Universities of Oldenburg, Göttingen, and Münster, the iDiv Leipzig and the Nationalpark Niedersächsisches Wattenmeer. Experimental islands and saltmarsh enclosed plots were created in the back barrier tidal flat and in the saltmarsh zone of the island of Spiekeroog. Meteorological data were collected near the experimental setup, with a locally installed weather station located approximately 500m north of the southern shoreline. The weather station system used here was a ClimaSensor US 4.920x.00.00x that was pre-calibrated by the manufacturer (Adolf Thies GmbH & Co. KG, D-Göttingen). Data were recorded and saved within the Processcontrol Weather (c) -4H- JENA engineering GmbH (v20.1.0.1 2020) software in a sampling interval of 1 min, with an averaging time of 10 s. Date and time were given in UTC and the position was derived from the internal GPS system. Data handling was performed according to Zielinski et al. (2018): Post-processing of collected data was done using MATLAB (R2018a). Quality control was performed by (a) erasing data covering maintenance activities, (b) removing outliers, defined as data exhibiting changes of more than two standard deviations within one time step, and (c) visually checks.
DOI: 10.1594/pangaea.873947
title: Track of GPS-Drifter ICBM_E1703_011 in the southern North Sea
DOI: 10.1594/pangaea.845705
title: Physical oceanography at the Jade Bay, tidal cycle, March 2015, transect A01
DOI: 10.21233/5zmm-cp72
title: RP-79 diatom surface sample dataset

description: Raw data for the RP-79 diatom surface sample dataset submitted to the Neotoma Paleoecology Database. Data is available through the landing page in JSON format. The landing page referenced by the DOI also contains links to publications and a map-based viewer for the dataset. The Neotoma Paleoecology Database maintains a homepage at https://www.neotomadb.org.
DOI: 10.1594/pangaea.973117
title: ADCP current measurements (600 kHz) from autonomous surface vehicle on 05.08.2023 during RV HEINCKE cruise HE626

description: Ocean velocities were collected by a Teledyne RD Instruments 600 kHz RiverRay ADCP that was mounted on an autonomous surface vehicle Halobates along a predefined transect pattern on August 5th 2023 during RV HEINCKE cruise HE626. The transducer was located at 0.257 m below the water line. The instrument was operated in single-ping, broadband mode with automatically selected bins (ranging from 0.1 - 0.8 m) depending on water depth and a blanking distance of 0.25 m. The velocity of Halobates was calculated from position fixes obtained by the Global Positioning System (GPS). Heading, pitch and roll data from vessel's gyrocompass and the navigation data were used by the data acquisition software ViSea DAS (AquaVision®) internally to convert ADCP velocities into earth coordinates. Accuracy of the ADCP velocities mainly depends on the quality of the position fixes and Halobates' heading data. Further errors stem from a misalignment of the transducer with Halobates' centerline.
DOI: 10.1594/pangaea.973694
title: Master tracks in different resolutions of HEINCKE cruise HE649, Bremerhaven - Bremerhaven, 2024-10-15 - 2024-10-27

description: Raw data acquired by position sensors on board RV Heincke during expedition HE649 were processed to receive a validated master track which can be used as reference of further expedition data. During HE649 the inertial navigation system IXSEA PHINS III and the GPS receivers Trimble Marine SPS461 and SAAB R5 SUPREME NAV were used as navigation sensors. Data were downloaded from DAVIS SHIP data base (https://dship.awi.de) with a resolution of 1 sec. Processed data are provided as a master track with 1 sec resolution derived from the position sensors' data selected by priority and a generalized track with a reduced set of the most significant positions of the master track.
description: This dataset contains the master track in 10 min resolution, for other resolutions please see "Other version" references.
DOI: 10.1594/pangaea.910166
title: Track of GPS-Drifter He520E06_D06 in the southern North Sea
DOI: 10.1594/pangaea.973124
title: Optical water quality variables (Secchi depth and Forel-Ule color indexes) observed during RV HEINCKE cruise HE609 from Bremerhaven, Germany to Bremerhaven, Germany

description: Water clarity and color were observed during the RV HEINCKE cruise HE609 (04.10.2022 to 26.10.2022), from Bremerhaven, Germany to Bremerhaven, Germany) using a white Secchi disc with a diameter of 40 cm and a Forel-Ule color scale. The Secchi depth (SD) was recorded as a relative measure of water clarity at each in situ station during day time. At half SD the apparent color of the water above the submerged Secchi disc was determined using the Forel-Ule color scale. A Forel-Ule color scale is a classic tools used to differentiate the percieved color of water based on a scale from 1 (indigo blue) to 21 (cola brown). The measurements were conducted as recemmend in literature (Garaba and Zielinski, 2015; Wernand, 2011; Wernand and van der Woerd, 2010).
DOI: 10.1594/pangaea.973126
title: Optical water quality variables (Secchi depth and Forel-Ule color indexes) observed during RV HEINCKE cruise HE614 from Bremerhaven, Germany to Bremerhaven, Germany

description: Water clarity and color were observed during the RV HEINCKE cruise HE614 (01.03.2023 to 21.03.2023), from Bremerhaven, Germany to Bremerhaven, Germany) using a white Secchi disc with a diameter of 40 cm and a Forel-Ule color scale. The Secchi depth (SD) was recorded as a relative measure of water clarity at each in situ station during day time. At half SD the apparent color of the water above the submerged Secchi disc was determined using the Forel-Ule color scale. A Forel-Ule color scale is a classic tools used to differentiate the percieved color of water based on a scale from 1 (indigo blue) to 21 (cola brown). The measurements were conducted as recemmend in literature (Garaba and Zielinski, 2015; Wernand, 2011; Wernand and van der Woerd, 2010).
DOI: 10.1594/pangaea.973128
title: Optical water quality variables (Secchi depth and Forel-Ule color indexes) observed during RV HEINCKE cruise HE626 from Bremerhaven, Germany to Bremerhaven, Germany

description: Water clarity and color were observed during the RV HEINCKE cruise HE626 (20.07.2023 - 09.08.2023, Wilhelmshaven, Germany - Wilhelmshaven, Germany) using a white Secchi disc with a diameter of 40 cm and a Forel-Ule color scale. The Secchi depth (SD) was recorded as a relative measure of water clarity at each in situ station during day time. At half SD the apparent color of the water above the submerged Secchi disc was determined using the Forel-Ule color scale. A Forel-Ule color scale is a classic tools used to differentiate the percieved color of water based on a scale from 1 (indigo blue) to 21 (cola brown). The measurements were conducted as recemmend in literature (Garaba and Zielinski, 2015; Wernand, 2011; Wernand and van der Woerd, 2010).
DOI: 10.1594/pangaea.973129
title: Optical water quality variables (Secchi depth and Forel-Ule color indexes) observed during RV HEINCKE cruise HE626-2 from Bremerhaven, Germany to Bremerhaven, Germany

description: Water clarity and color were observed during the RV HEINCKE cruise HE626-2 (27.10.2023 - 01.11.2023, Wilhelmshaven, Germany - Wilhelmshaven, Germany) using a white Secchi disc with a diameter of 40 cm and a Forel-Ule color scale. The Secchi depth (SD) was recorded as a relative measure of water clarity at each in situ station during day time. At half SD the apparent color of the water above the submerged Secchi disc was determined using the Forel-Ule color scale. A Forel-Ule color scale is a classic tools used to differentiate the percieved color of water based on a scale from 1 (indigo blue) to 21 (cola brown). The measurements were conducted as recemmend in literature (Garaba and Zielinski, 2015; Wernand, 2011; Wernand and van der Woerd, 2010).
DOI: 10.1594/pangaea.843735
title: Pressure and processed water levels from the Time Series Station Spiekeroog in 2007
DOI: 10.21233/bkk5-j250
title: Beaver River ostracode surface sample dataset

description: Raw data for the Beaver River ostracode surface sample dataset submitted to the Neotoma Paleoecology Database. Data is available through the landing page in JSON format. The landing page referenced by the DOI also contains links to publications and a map-based viewer for the dataset. The Neotoma Paleoecology Database maintains a homepage at https://www.neotomadb.org.
DOI: 10.21233/yjhg-b425
title: Chesapeake Bay (MD99-2209) pollen dataset

description: Raw data for the Chesapeake Bay (MD99-2209) pollen dataset submitted to the Neotoma Paleoecology Database. Data is available through the landing page in JSON format. The landing page referenced by the DOI also contains links to publications and a map-based viewer for the dataset. The Neotoma Paleoecology Database maintains a homepage at https://www.neotomadb.org.
DOI: 10.1594/pangaea.968754
title: A global soil moisture product at 1 km resolution based on Sentinel-1 (2016-2022)

description: Soil moisture, although a small fraction of total water content, plays a critical role in the Earth's surface water-heat cycle by influencing processes such as evaporation, infiltration, and vegetation growth and development. Remote sensing has emerged as a critical method for obtaining global-scale soil moisture data. A dual-polarization algorithm (DPA) is proposed and the dual-polarization (VV+VH) observations from the Sentinel-1 C-band synthetic aperture radar are used to generate a global soil moisture dataset with a spatial resolution of 1 km. Due to the observation mode of Sentinel-1, the temporal resolution of this dataset is higher in European and high latitude regions compared to other continents and lower latitude regions. The dataset is provided in raster format, with one set of ascending and one set of descending data for each day, and to ensure data quality, certain areas not suitable for soil moisture retrieval have been excluded, such as water bodies, permanent wetlands, frozen areas, ice and snow covered surfaces, and urban and built-up areas. Feedback and collaboration to improve the dataset is encouraged.
description: * File descriptions: (1) File format: TIFF(2) Naming rule: SM_Ascending/Descending_YYYYMMDD.tif (eg: SM_D_20160906.tif)(3) Spatial resolution: 1km (about 0.0089831528 degree)(4) Columns and rows: 40074 and 20036(5) Coordinate system: D_WGS_1984 (EPSG:4326)(6) Scope: Top 89.9887335867, Left -179.990941903, Right 179.990941903, Bottom -89.9887335867(7) Pixel_Type: signed integer (16Bit)(8) Scale: 1000(9) Valid range: 0.02 to 0.6 m³/m³(10) Backgroud value:32767: Permanent Wetlands, Urban and Built-up Lands, Permanent Snow and Ice, Water Bodies32766: Surface temperature &lt; 275.15K32765: Snow cover &gt; 10%
DOI: 10.1594/pangaea.873900
title: Physical oceanography measurements in the tidal inlet between the islands Spiekeroog and Langeoog, Wadden Sea, North Sea, 2017-03

description: The data were measured in the German North Sea between the East-Frisian Islands Spiekeroog and Langeoog with RB Otzum (ICBM) on March 14 and 16 2017. Conductivity, temperature and pressure were measured by means of a Seabird CTD (type 19plusV2). On March 14 2017 data were collected for an entire tidal cycle, starting at low tide; whereas on March 16 2017 we measured only a half tidal cycle, starting at high tide. The profiles were taken in the middle of the tidal inlet between the two islands. During the CTD cast, where the CTD was veered with a speed of around 0.1 m/s, the boat was drifting with the current. The positions and times given in the data set mark the beginning of each CTD cast. Dates and times are given in UTC. The data were transformed by using the SBE Data Processing Software. Only the downcast profile was used and a bin average (binsize = 0.1 m) was calculated with the software.
DOI: 10.1594/pangaea.785566
title: Physical oceanography during HEINCKE cruise HE350
DOI: 10.1594/pangaea.944740
title: Continuous thermosalinograph oceanography along RV HEINCKE cruise track HE586

description: Raw data acquired by an SBE21 thermosalinograph and an auxiliary SBE38 temperature sensor (Sea-Bird Scientific, USA) installed in an underway seawater flow-through system on board RV Heincke were processed to yield a calibrated and validated data set of seawater temperature and salinity along the cruise track. The seawater inlet is located at a depth of 2 m. The raw hexadecimal data were downloaded from the DAVIS SHIP data base (https://dship.awi.de) at a resolution of 1 s, and converted to temperature and conductivity using the pre-deployment factory calibration coefficients. The converted data were averaged to 1 min values, outliers were removed, and sensor drift was corrected using coefficients obtained from a post-season calibration performed at Sea-Bird at the end of the measurement season. Salinity was calculated from internal temperature, conductivity and pressure according to the PSS-78 Practical Salinity Scale. Processed data are provided as 1 min means of seawater temperature, conductivity and salinity, aligned with position data taken from the master track. Quality flags are appended according to the SeaDataNet Data Quality Control Procedures (version from May 2010). More details are described in the attached processing report.
DOI: 10.1594/pangaea.930421
title: Physical oceanography during HEINCKE cruise HE563

description: Conductivity-temperature-depth profiles were measured using a Seabird SBE 911plus CTD during RV Heincke cruise HE563 between 06.10.2020 and 20.10.2020. Additional sensors included a WET Labs C-Star transmissometer and a WET Labs ECO-AFL fluorometer. Data were connected to the station book of the specific cruise as available in the DSHIP database. Processing of the data including removal of obvious outliers followed the procedures described in CTD Processing Logbook of RV Heincke (hdl:10013/epic.47427). A detailed report on the CTD data of HE563 is available at hdl:10013/epic.0f64128b-c704-4ef8-88d5-bfb82a2c5839.
DOI: 10.1594/pangaea.965123
title: Hyperspectral downward irradiance in water (Ed) measured during the cruise SO290 with RV SONNE

description: Data presented here were collected during the cruise SO290 with RV SONNE from Nuoméa (New Caledonia) to Nuoméa (New Caledonia) (April 15, 2022 - Mai, 12, 2022). In total, 19 underwater light profiles were collected at 7 stations, using a free-falling hyperspectral light profiler. The system used was a SEABIRD HyperPro II (SN 099, former Satlantic), equipped with a irradiance sensor to measure downward irradiance in water (Ed, SN 262) and a radiance sensor for the upward radiance in water (Lu, SN 227). A reference unit was attached to the ship to measure the downward irradiance in air (Es, SN 223). The sensors were pre-calibrated by the manufacturer and validated prior to the cruise with a reference lamp. Data were recorded with the SatView software (V 2.9.5_7) and processed from raw to Level1, 1b, 2, 2s to Level 3a using the ProSoft Processing software (V 7.7.19_2). Measured data were binned in 0.5 m depth intervals. A dark correction was made automatically based on shutter measurements by the instrument. Measurements with a tilt higher than 5 were not taken into account during processing. Spectra were interpolated to 1 nm intervals. For each station the hyperspectral profiles for each parameter cover the wavelength range from 400-700 nm, for Ed and Es in [W/m nm], for Lu in [W/m nm sr]. For Ed, Lu and Es descriptive statistics are given including min, max, mean, median and standard deviation of the tilt and the photosynthetically active radiation PAR [µmol photons/m² s (sr)], integrated from 400 - 700 nm. To allow an assignment of above water conditions to the respective depth measurements, Es spectra were given as a function of depth, recalculated from data Level2s. The Profiler measurements were only conducted during daylight. Raw data are available on request from the principal investigator.
DOI: 10.21233/3b1g-2z05
title: Qizimeishan testate amoebae surface sample dataset

description: Raw data for the Qizimeishan testate amoebae surface sample dataset submitted to the Neotoma Paleoecology Database. Data is available through the landing page in JSON format. The landing page referenced by the DOI also contains links to publications and a map-based viewer for the dataset. The Neotoma Paleoecology Database maintains a homepage at https://www.neotomadb.org.
DOI: 10.1594/pangaea.843734
title: Pressure and processed water levels from the Time Series Station Spiekeroog in 2006
DOI: 10.1594/pangaea.825422
title: Physical oceanography during HEINCKE cruise HE410/1
DOI: 10.1594/pangaea.902153
title: Physical oceanography during HEINCKE cruise HE527
DOI: 10.1594/pangaea.873945
title: Track of GPS-Drifter ICBM_E1703_009 in the southern North Sea
DOI: 10.21233/svzk-xh82
title: LDDsite5553 ostracode surface sample dataset

description: Raw data for the LDDsite5553 ostracode surface sample dataset submitted to the Neotoma Paleoecology Database. Data is available through the landing page in JSON format. The landing page referenced by the DOI also contains links to publications and a map-based viewer for the dataset. The Neotoma Paleoecology Database maintains a homepage at https://www.neotomadb.org.
DOI: 10.57841/casdc.0005451
title: 水稻籽粒重金属低积累的分子网络二
DOI: 10.1594/pangaea.785577
title: Physical oceanography during HEINCKE cruise HE366
DOI: 10.1594/pangaea.824704
title: Physical oceanography during HEINCKE cruise HE410/2
DOI: 10.1594/pangaea.859733
title: Continuous thermosalinograph oceanography along HEINCKE cruise track HE366
DOI: 10.1594/pangaea.959701
title: Physical oceanography during RV SONNE cruise SO290 (PaläoTaNZ)

description: Data presented here were collected during the cruise SO290 (PaläoTaNZ) with RV Sonne from Nouméa, New Caledonia to Nouméa, New Caledonia (April, 11th, 2022 to May 12th, 2022). In total, 21 vertical deep CTD-hauls were conducted. The CTD system used was a Sea-Bird Electronics Inc. SBE 911plus probe (SN 09-1266). The CTD was attached to a SBE 32 Carousel Water Sampler (SN 32-1119) containing 24 20-liter Ocean Test Equipment Inc. bottles. The system was equipped with double temperature (SBE 3) and conductivity sensors (SBE 4), a pressure sensor (Digiquartz) an oxygen Optode (Aanderaa Optode 4831F), an altimeter (Benthos), and a chlorophyll fluorometer combined with a turbidity sensor (WET Labs ECO_AFL FL). The sensors were pre-calibrated by the manufacturers. Data were recorded with the Seasave V 7.26.7.107 software and processed using the SeaBird SBE Data Processing. Data were despiked, filtered, bin averaged (size 0.5 m) and also visually checked. The ship position was derived from the shipboard GPS-system linked to the CTD data. The time zone is given in UTC. Salinity was quality checked by reference samples [n=16], measured with an Optimare Precision Salinometer (OPS) after the cruise (S1: R² 1, S2: R² 1). Samples for oxygen [n=103] were measured in the lab by Winkler titration to correct values of the Oxygen Optode (R² 0.97). Raw data on request.
DOI: 10.1594/pangaea.810455
title: Physical oceanography during HEINCKE cruise HE389
DOI: 10.1594/pangaea.937519
title: Mesozooplankton biovolume per size class and station from POLARSTERN (ANT-XXXIII/3) cruise PS112 (dataset 4)
DOI: 10.1594/pangaea.840689
title: Station list and links to master tracks in different resolutions of HEINCKE cruise HE435
DOI: 10.1594/pangaea.845707
title: Physical oceanography at the Jade Bay, tidal cycle, March 2015, transect B
DOI: 10.1594/pangaea.910161
title: Track of GPS-Drifter HE520E00_D01 in the southern North Sea
DOI: 10.1594/pangaea.910162
title: Track of GPS-Drifter HE520E01_D02 in the southern North Sea
DOI: 10.1594/pangaea.843668
title: Station list and links to master tracks in different resolutions of HEINCKE cruise HE338, Bremerhaven - Bremerhaven, 2010-10-05 - 2010-10-11
DOI: 10.1594/pangaea.843641
title: Station list and links to master tracks in different resolutions of HEINCKE cruise HE268, Bremerhaven - Bremerhaven, 2007-05-10 - 2007-05-15
DOI: 10.1594/pangaea.910172
title: Track of GPS-Drifter He520E15_D14 in the southern North Sea
DOI: 10.21233/jk7v-yf24
title: Big Boy Canyon plant macrofossil dataset

description: Raw data for the Big Boy Canyon plant macrofossil dataset submitted to the Neotoma Paleoecology Database. Data is available through the landing page in JSON format. The landing page referenced by the DOI also contains links to publications and a map-based viewer for the dataset. The Neotoma Paleoecology Database maintains a homepage at https://www.neotomadb.org.
DOI: 10.1594/pangaea.886242
title: Links to master tracks in different resolutions of HEINCKE cruise HE498, Bremerhaven - Bremerhaven, 2017-10-06 - 2017-10-13
DOI: 10.1594/pangaea.966773
title: Continuous meteorological observations at DynaCom automatic weather station, Spiekeroog, Germany, 2023-01

description: Data presented here were collected between January 2022 to December 2023 within the research unit DynaCom (Spatial community ecology in highly dynamic landscapes: From island biogeography to metaecosystems, https://uol.de/dynacom/ ) of the Universities of Oldenburg, Göttingen, and Münster, the iDiv Leipzig and the Nationalpark Niedersächsisches Wattenmeer. Experimental islands and saltmarsh enclosed plots were created in the back barrier tidal flat and in the saltmarsh zone of the island of Spiekeroog. Meteorological data were collected near the experimental setup, with a locally installed weather station located approximately 500m north of the southern shoreline. The weather station system used here was a ClimaSensor US 4.920x.00.00x that was pre-calibrated by the manufacturer (Adolf Thies GmbH & Co. KG, D-Göttingen). Data were recorded and saved within the Processcontrol Weather (c) -4H- JENA engineering GmbH (v20.1.0.1 2020) software in a sampling interval of 1 min, with an averaging time of 10 s. Date and time were given in UTC and the position was derived from the internal GPS system. Data handling was performed according to Zielinski et al. (2018): Post-processing of collected data was done using MATLAB (R2018a). Quality control was performed by (a) erasing data covering maintenance activities, (b) removing outliers, defined as data exhibiting changes of more than two standard deviations within one time step, and (c) visually checks.