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  • 1
  • 2
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    AtlantOS
    In:  AtlantOS Deliverable, D3.6 . AtlantOS, 8 pp.
    Publication Date: 2017-09-19
    Description: D3.6 Glider App for public dissemination and outreach: Primarily developed for outreach purposes the application will also include some functionality for glider pilots. The App will interface in realtime with glider communication stations on land. Functionality will be based and tested on planned glider missions by SAMS partner and will then be rolled out to other partners.
    Type: Report , NonPeerReviewed , info:eu-repo/semantics/book
    Format: text
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  • 3
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2024-01-22
    Description: Snow height was measured by the Snow Buoy 2019S91, an autonomous platform, installed on drifting sea ice in the Arctic Ocean during RV Araon 2019. The resulting time series describes the evolution of snow height as a function of place and time between 13 August 2019 and 25 August 2019 in sample intervals of 1 hour. The Snow Buoy consists of four independent acoustic range finder measurements representing the area (approx. 10 m**2) around the buoy. In addition to snow height, geographic position (GPS), barometric pressure, air temperature, and surface temperature were measured. Negative values of snow height occur if surface ablation continues into the sea ice. Thus, these measurements describe the position of the sea ice surface relative to the original snow-ice interface. Differences between single sensors indicate small-scale variability of the snow pack around the buoy.
    Keywords: 2019S91; Araon2019/1; autonomous platform; AWI_SeaIce; buoy; BUOY_SNOW; Current sea ice maps for Arctic and Antarctic; DATE/TIME; drift; Global positioning system, time since last fix; LATITUDE; LONGITUDE; meereisportal.de; MIDO; Multidisciplinary Ice-based Distributed Observatory; Pressure, atmospheric; Quality flag, air temperature; Quality flag, atmospheric pressure; Quality flag, position; Quality flag, snow height; Quality flag, technical temperature; Sea Ice Physics @ AWI; Snow buoy; snow depth; Snow height; Temperature, air; Temperature, technical
    Type: Dataset
    Format: text/tab-separated-values, 4560 data points
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  • 4
    Publication Date: 2024-04-20
    Description: This dataset contains hydroacoustic measurements collected by an autonomous ice-tethered bio-physical observatory during its drift across the Central Arctic Ocean from the end of MOSAiC in September 2020 to the next spring in May 2021. The measurements were performed by an Acoustic Zooplankton and Fish Profiler (AZFP, ASL) with factory calibrations. Data are provided as volume backscatter (Sv, in dB re 1 m⁻¹). We provide data for the frequencies 67, 125, 200 and 455 kHz. These files contain the quality-controlled raw data. The data were cleaned, processed and analysed in the paper Sea-ice decline makes zooplankton stay deeper for longer by Flores, Veyssiere et al. (submitted to Nature Cliimate Change), which contains a detailed description of the instrument and the measurement settings. The format can be readily ingested in the hydroacoustic data processing application EchoView.
    Keywords: 2020AZFP1; Acoustical Zoological Fish Profiler; Arctic_PASSION; Arctic Ocean; AZFP; Binary Object; central Arctic Ocean; DATE/TIME; ECOLIGHT; Ecosystem functions controlled by sea ice and light in a changing Arctic; File content; FRAM; FRontiers in Arctic marine Monitoring; Hydroacoustic backscatter; LATITUDE; LONGITUDE; MIDO; Mosaic; MOSAiC; MOSAIC_PO; MOSAiC20192020; Multidisciplinary drifting Observatory for the Study of Arctic Climate; Multidisciplinary Ice-based Distributed Observatory; Pan-Arctic observing System of Systems: Implementing Observations for societal Needs; Polarstern; PS122/5; PS122/5_58-163; vertical migration; Zooplankton
    Type: Dataset
    Format: text/tab-separated-values, 8 data points
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  • 5
    Publication Date: 2021-01-12
    Description: The radiative transfer of shortwave solar radiation through the sea ice cover of the polar oceans is a crucial aspect of energy partitioning at the atmosphere–ice–ocean interface. A detailed understanding of how sunlight is reflected and transmitted by the sea ice cover is needed for an accurate representation of critical processes in climate and ecosystem models, such as the ice–albedo feedback. Due to the challenges associated with ice internal measurements, most information about radiative transfer in sea ice has been gained by optical measurements above and below the sea ice. To improve our understanding of radiative transfer processes within the ice itself, we developed a new kind of instrument equipped with a number of multispectral light sensors that can be frozen into the ice. A first prototype consisting of a 2.3 m long chain of 48 sideward planar irradiance sensors with a vertical spacing of 0.05 m was deployed at the geographic North Pole in late August 2018, providing autonomous, vertically resolved light measurements within the ice cover during the autumn season. Here we present the first results of this instrument, discuss the advantages and application of the prototype, and provide first new insights into the spatiotemporal aspect of radiative transfer within the sea ice itself. In particular, we investigate how measured attenuation coefficients relate to the optical properties of the ice pack and show that sideward planar irradiance measurements are equivalent to measurements of total scalar irradiance.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
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  • 6
    Publication Date: 2021-02-08
    Description: The radiative transfer of short-wave solar radiation through the sea ice cover of the polar oceans is a crucial aspect of energy partitioning at the atmosphere-ice-ocean interface. A detailed understanding of how sunlight is reflected, absorbed and transmitted by the sea ice cover is needed for an accurate representation of critical processes in climate and ecosystem models, such as the ice-albedo feedback. Due to the challenges associated with ice internal measurements, most information about radiative transfer in sea ice has been gained by optical measurements above and below the sea ice. To improve our understanding of radiative transfer processes within the ice itself, we developed an innovative, chain-type instrument equipped with up to 64 multispectral light sensors that can be frozen into the ice. Here we present the results of a first prototype deployment at the North Pole in fall of 2018, as well as recently acquired data from the MOSAiC drift expedition in spring and summer 2020. We discuss the advantages, application, and limits of the device and provide first new insights into the spatiotemporal aspect of radiative transfer within the sea ice itself. In particular, we investigate how measured attenuation coefficients relate to the optical properties of the ice pack, and show that sideward planar irradiance measurements are equivalent to measurements of total scalar irradiance. We also show how this light sensor chain can be used for assessment of the temporal evolution in ice algal biomass and water column properties.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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  • 7
    Publication Date: 2022-05-25
    Description: © The Author(s), 2017. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Elementa Science of the Anthropocene 5 (2017): 47, doi:10.1525/elementa.233.
    Description: An array of novel directional wavebuoys was designed and deployed into the Beaufort Sea ice cover in March 2014, as part of the Office of Naval Research Marginal Ice Zone experiment. The buoys were designed to drift with the ice throughout the year and monitor the expected breakup and retreat of the ice cover, forced by waves travelling into the ice from open water. Buoys were deployed from fast-and-light air-supported ice camps, based out of Sachs Harbour on Canada’s Banks Island, and drifted westwards with the sea ice over the course of spring, summer and autumn, as the ice melted, broke up and finally re-froze. The buoys transmitted heave, roll and pitch timeseries at 1 Hz sample frequency over the course of up to eight months, surviving both convergent ice dynamics and significant waves-in-ice events. Twelve of the 19 buoys survived until their batteries were finally exhausted during freeze-up in late October/November. Ice impact was found to have contaminated a significant proportion of the Kalman-filter-derived heave records, and these bad records were removed with reference to raw x/y/z accelerations. The quality of magnetometer-derived buoy headings at the very high magnetic field inclinations close to the magnetic pole was found to be generally acceptable, except in the case of four buoys which had probably suffered rough handling during transport to the ice. In general, these new buoys performed as expected, though vigilance as to the veracity of the output is required.
    Description: The work formed part of the Office of Naval Research “Marginal Ice Zone” Departmental Research Initiative. Authors were supported by Grant Numbers N000141210130 (Wadhams and Doble), N000141210359 (Wilkinson, Maksym and Hwang).
    Keywords: Sea-ice ; Waves ; Arctic 
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 8
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    In:  EPIC3International Symposium on Sea Ice at the Interface, Winnipeg, MA, Canada, 2019-08-19-2019-08-23
    Publication Date: 2019-10-30
    Description: The quantity and quality of sunlight transmitted into and through sea ice is a crucial key necessary to understand the thermodynamic development of the ice cover, upper ocean heat and freshwater budget, as well as the associated primary production. Due to its solid impenetrable nature, most optical measurements so far have been conducted above and underneath the sea ice covering our polar oceans. Only very limited measurements have been carried out inside the ice cover itself. This strongly limits our current knowledge of the vertically varying inherent optical properties (IOP) of sea ice, as well as the geometric shape of the in-ice light field. Both factors currently limit our abilities to reliably model radiative transfer in sea ice. Here we present multiple new tools that can fill this observational gap and provide comprehensive optical measurements within the ice: This includes a chain of multispectral light sensors for seasonal long-term monitoring. It is derived from the proven design of the newest generation of ice-mass-balance buoys with digital thermistor strings and enables a non-destructive measurement with flexible geometry. We present data from a first prototype deployed together with an array of drifting ice observatories at the North Pole in September 2018. These vertically resolved in-ice light profiles are compared to in-ice measurements with a newly designed in-ice optical profiler system based on the well-proven TriOS Ramses hyperspectral radiometers. Combining expertise from photonics, medical and sea-ice science enables the ongoing development of a set of endoscopic probes allowing optical studies in sea ice with minimum disturbance of the ice. This includes in-ice microscopy for in-situ ice algal investigations, a UV-spectrometer to observe brine nitrate concentration in situ, a reflectance probe for high-resolution direct determination of inherent optical properties, as well as a radiance camera for quantification of the angular radiance distribution. Here we present data from the first field tests during the Arctic field season 2018. First ruggedized prototypes could be available to the scientific community soon.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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  • 9
    Publication Date: 2022-06-22
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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  • 10
    Publication Date: 2022-06-22
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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