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  • 1
    Publication Date: 2024-02-15
    Description: This dataset contains CTD measurements taken in 2015, 2016, 2017, 2018, 2019, 2022, and 2023 during expeditions to Herschel Island - Qikiqtaruk, Yukon, Canada. For the data recording a CTD CastAway was used. The sampling was conducted from a boat from which the CTD was lowered to the sea floor at the specific sampling sites. The sampling information encompasses the GPS position, water depth, pressure, temperature, electrical conductivity, specific conductance, and salinity.
    Keywords: AWI_PerDyn; AWI_Perma; AWI Arctic Land Expedition; CA-Land_2015_YukonCoast; CA-Land_2015_YukonCoast_CTD_001; CA-Land_2015_YukonCoast_CTD_002; CA-Land_2015_YukonCoast_CTD_003; CA-Land_2015_YukonCoast_CTD_004; CA-Land_2015_YukonCoast_CTD_005; CA-Land_2015_YukonCoast_CTD_006; CA-Land_2015_YukonCoast_CTD_007; CA-Land_2015_YukonCoast_CTD_008; CA-Land_2015_YukonCoast_CTD_009; CA-Land_2015_YukonCoast_CTD_010; CA-Land_2015_YukonCoast_CTD_011; CA-Land_2015_YukonCoast_CTD_012; CA-Land_2015_YukonCoast_CTD_013; CA-Land_2015_YukonCoast_CTD_014; CA-Land_2015_YukonCoast_CTD_015; CA-Land_2015_YukonCoast_CTD_016; CA-Land_2015_YukonCoast_CTD_017; CA-Land_2015_YukonCoast_CTD_018; CA-Land_2015_YukonCoast_CTD_019; CA-Land_2015_YukonCoast_CTD_020; CA-Land_2015_YukonCoast_CTD_021; CA-Land_2015_YukonCoast_CTD_022; CA-Land_2015_YukonCoast_CTD_023; CA-Land_2015_YukonCoast_CTD_024; CA-Land_2015_YukonCoast_CTD_025; CA-Land_2016_YukonCoast_CTD_001; CA-Land_2016_YukonCoast_CTD_002; CA-Land_2016_YukonCoast_CTD_003; CA-Land_2016_YukonCoast_CTD_004; CA-Land_2016_YukonCoast_CTD_005; CA-Land_2016_YukonCoast_CTD_006; CA-Land_2016_YukonCoast_CTD_007; CA-Land_2016_YukonCoast_CTD_008; CA-Land_2016_YukonCoast_CTD_009; CA-Land_2016_YukonCoast_spring; CA-Land_2017_YukonCoast; CA-Land_2017_YukonCoast_CTD_001; CA-Land_2017_YukonCoast_CTD_002; CA-Land_2017_YukonCoast_CTD_003; CA-Land_2017_YukonCoast_CTD_004; CA-Land_2017_YukonCoast_CTD_005; CA-Land_2017_YukonCoast_CTD_006; CA-Land_2017_YukonCoast_CTD_007; CA-Land_2017_YukonCoast_CTD_008; CA-Land_2017_YukonCoast_CTD_009; CA-Land_2017_YukonCoast_CTD_010; CA-Land_2017_YukonCoast_CTD_011; CA-Land_2017_YukonCoast_CTD_012; CA-Land_2017_YukonCoast_CTD_013; CA-Land_2017_YukonCoast_CTD_014; CA-Land_2017_YukonCoast_CTD_015; CA-Land_2017_YukonCoast_CTD_016; CA-Land_2017_YukonCoast_CTD_017; CA-Land_2017_YukonCoast_CTD_018; CA-Land_2017_YukonCoast_CTD_019; CA-Land_2017_YukonCoast_CTD_020; CA-Land_2017_YukonCoast_CTD_021; CA-Land_2017_YukonCoast_CTD_022; CA-Land_2017_YukonCoast_CTD_023; CA-Land_2017_YukonCoast_CTD_024; CA-Land_2017_YukonCoast_CTD_025; CA-Land_2017_YukonCoast_CTD_026; CA-Land_2017_YukonCoast_CTD_027; CA-Land_2017_YukonCoast_CTD_028; CA-Land_2017_YukonCoast_CTD_029; CA-Land_2017_YukonCoast_CTD_030; CA-Land_2017_YukonCoast_CTD_031; CA-Land_2017_YukonCoast_CTD_032; CA-Land_2017_YukonCoast_CTD_033; CA-Land_2017_YukonCoast_CTD_034; CA-Land_2017_YukonCoast_CTD_035; CA-Land_2017_YukonCoast_CTD_036; CA-Land_2017_YukonCoast_CTD_037; CA-Land_2017_YukonCoast_CTD_038; CA-Land_2017_YukonCoast_CTD_039; CA-Land_2017_YukonCoast_CTD_040; CA-Land_2017_YukonCoast_CTD_041; CA-Land_2017_YukonCoast_CTD_042; CA-Land_2017_YukonCoast_CTD_043; CA-Land_2017_YukonCoast_CTD_044; CA-Land_2017_YukonCoast_CTD_045; CA-Land_2017_YukonCoast_CTD_046; CA-Land_2017_YukonCoast_CTD_047; CA-Land_2018_YukonCoast; CA-Land_2018_YukonCoast_CTD_003; CA-Land_2018_YukonCoast_CTD_004; CA-Land_2018_YukonCoast_CTD_005; CA-Land_2018_YukonCoast_CTD_006; CA-Land_2019_YukonCoast_CTD_002; CA-Land_2019_YukonCoast_CTD_003; CA-Land_2019_YukonCoast_CTD_004; CA-Land_2019_YukonCoast_CTD_005; CA-Land_2019_YukonCoast_CTD_006; CA-Land_2019_YukonCoast_CTD_007; CA-Land_2019_YukonCoast_CTD_008; CA-Land_2019_YukonCoast_CTD_009; CA-Land_2019_YukonCoast_CTD_010; CA-Land_2019_YukonCoast_CTD_011; CA-Land_2019_YukonCoast_CTD_012; CA-Land_2019_YukonCoast_CTD_013; CA-Land_2019_YukonCoast_CTD_014; CA-Land_2019_YukonCoast_CTD_015; CA-Land_2019_YukonCoast_CTD_016; CA-Land_2019_YukonCoast_CTD_017; CA-Land_2019_YukonCoast_CTD_018; CA-Land_2019_YukonCoast_CTD_019; CA-Land_2019_YukonCoast_CTD_020; CA-Land_2019_YukonCoast_CTD_021; CA-Land_2019_YukonCoast_CTD_022; CA-Land_2019_YukonCoast_CTD_023; CA-Land_2019_YukonCoast_CTD_024; CA-Land_2019_YukonCoast_CTD_025; CA-Land_2019_YukonCoast_CTD_026; CA-Land_2019_YukonCoast_CTD_027; CA-Land_2019_YukonCoast_CTD_028; CA-Land_2019_YukonCoast_CTD_029; CA-Land_2019_YukonCoast_CTD_030; CA-Land_2019_YukonCoast_CTD_031; CA-Land_2019_YukonCoast_CTD_032; CA-Land_2019_YukonCoast_CTD_033; CA-Land_2019_YukonCoast_CTD_034; CA-Land_2019_YukonCoast_CTD_035; CA-Land_2019_YukonCoast_CTD_036; CA-Land_2019_YukonCoast_CTD_037; CA-Land_2019_YukonCoast_CTD_038; CA-Land_2019_YukonCoast_CTD_039; CA-Land_2019_YukonCoast_CTD_040; CA-Land_2019_YukonCoast_CTD_041; CA-Land_2019_YukonCoast_CTD_042; CA-Land_2019_YukonCoast_CTD_043; CA-Land_2019_YukonCoast_CTD_044; CA-Land_2019_YukonCoast_CTD_045; CA-Land_2019_YukonCoast_CTD_046; CA-Land_2019_YukonCoast_CTD_047; CA-Land_2019_YukonCoast_CTD_048; CA-Land_2019_YukonCoast_CTD_049; CA-Land_2019_YukonCoast_CTD_050; CA-Land_2019_YukonCoast_CTD_051; CA-Land_2019_YukonCoast_CTD_052; CA-Land_2019_YukonCoast_CTD_053; CA-Land_2019_YukonCoast_spring; CA-Land_2022_YukonCoast; CA-Land_2022_YukonCoast_CTD_001; CA-Land_2022_YukonCoast_CTD_002; CA-Land_2022_YukonCoast_CTD_003; CA-Land_2022_YukonCoast_CTD_004; CA-Land_2022_YukonCoast_CTD_005; CA-Land_2022_YukonCoast_CTD_006; CA-Land_2022_YukonCoast_CTD_007; CA-Land_2022_YukonCoast_CTD_008; CA-Land_2022_YukonCoast_CTD_009; CA-Land_2022_YukonCoast_CTD_010; CA-Land_2022_YukonCoast_CTD_011; CA-Land_2022_YukonCoast_CTD_012; CA-Land_2022_YukonCoast_CTD_013; CA-Land_2022_YukonCoast_CTD_014; CA-Land_2022_YukonCoast_CTD_015; CA-Land_2022_YukonCoast_CTD_016; CA-Land_2022_YukonCoast_CTD_017; CA-Land_2022_YukonCoast_CTD_018; CA-Land_2022_YukonCoast_CTD_019; CA-Land_2022_YukonCoast_CTD_020; CA-Land_2022_YukonCoast_CTD_021; CA-Land_2022_YukonCoast_CTD_022; CA-Land_2022_YukonCoast_CTD_023; CA-Land_2022_YukonCoast_CTD_024; CA-Land_2022_YukonCoast_CTD_025; CA-Land_2022_YukonCoast_CTD_026; CA-Land_2022_YukonCoast_CTD_027; CA-Land_2022_YukonCoast_CTD_028; CA-Land_2022_YukonCoast_CTD_029; CA-Land_2022_YukonCoast_CTD_030; CA-Land_2022_YukonCoast_CTD_031; CA-Land_2022_YukonCoast_CTD_032; CA-Land_2022_YukonCoast_CTD_033; CA-Land_2022_YukonCoast_CTD_034; CA-Land_2022_YukonCoast_CTD_035; CA-Land_2022_YukonCoast_CTD_036; CA-Land_2022_YukonCoast_CTD_037; CA-Land_2022_YukonCoast_CTD_038; CA-Land_2022_YukonCoast_CTD_039; CA-Land_2022_YukonCoast_CTD_040; CA-Land_2022_YukonCoast_CTD_041; CA-Land_2022_YukonCoast_CTD_042; CA-Land_2022_YukonCoast_CTD_043; CA-Land_2022_YukonCoast_CTD_044; CA-Land_2022_YukonCoast_CTD_045; CA-Land_2022_YukonCoast_CTD_046; CA-Land_2022_YukonCoast_CTD_047; CA-Land_2022_YukonCoast_CTD_048; CA-Land_2022_YukonCoast_CTD_049; CA-Land_2022_YukonCoast_CTD_050; CA-Land_2022_YukonCoast_CTD_051; CA-Land_2022_YukonCoast_CTD_052; CA-Land_2022_YukonCoast_CTD_053; CA-Land_2022_YukonCoast_CTD_054; CA-Land_2022_YukonCoast_CTD_055; CA-Land_2022_YukonCoast_CTD_056; CA-Land_2022_YukonCoast_CTD_057; CA-Land_2022_YukonCoast_CTD_058; CA-Land_2022_YukonCoast_CTD_059; CA-Land_2022_YukonCoast_CTD_060; CA-Land_2022_YukonCoast_CTD_061; CA-Land_2022_YukonCoast_CTD_062; CA-Land_2022_YukonCoast_CTD_063; CA-Land_2022_YukonCoast_CTD_064; CA-Land_2022_YukonCoast_CTD_065; CA-Land_2022_YukonCoast_CTD_066; CA-Land_2022_YukonCoast_CTD_067; CA-Land_2022_YukonCoast_CTD_068; CA-Land_2022_YukonCoast_CTD_069; CA-Land_2022_YukonCoast_CTD_070; CA-Land_2022_YukonCoast_CTD_071; CA-Land_2022_YukonCoast_CTD_072; CA-Land_2022_YukonCoast_CTD_073; CA-Land_2022_YukonCoast_CTD_074; CA-Land_2022_YukonCoast_CTD_075; CA-Land_2022_YukonCoast_CTD_076; CA-Land_2022_YukonCoast_CTD_077; CA-Land_2022_YukonCoast_CTD_078; CA-Land_2022_YukonCoast_CTD_079; CA-Land_2022_YukonCoast_CTD_080; CA-Land_2022_YukonCoast_CTD_081; CA-Land_2022_YukonCoast_CTD_082; CA-Land_2022_YukonCoast_CTD_083; CA-Land_2022_YukonCoast_CTD_084; CA-Land_2022_YukonCoast_CTD_085; CA-Land_2022_YukonCoast_CTD_086; CA-Land_2022_YukonCoast_CTD_087; CA-Land_2022_YukonCoast_CTD_088; CA-Land_2022_YukonCoast_CTD_089; CA-Land_2022_YukonCoast_CTD_090; CA-Land_2022_YukonCoast_CTD_091; CA-Land_2022_YukonCoast_CTD_092; CA-Land_2022_YukonCoast_CTD_093; CA-Land_2022_YukonCoast_CTD_094; CA-Land_2022_YukonCoast_CTD_095; CA-Land_2022_YukonCoast_CTD_096; CA-Land_2022_YukonCoast_CTD_097; CA-Land_2022_YukonCoast_CTD_098; CA-
    Type: Dataset
    Format: text/tab-separated-values, 71589 data points
    Location Call Number Expected Availability
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  • 2
    Publication Date: 2024-02-17
    Description: Fieldwork was conducted in July 2022 in the coastal waters around Herschel Island - Qikiqtaruk, Canada. Seven sampling days were carried out in two consecutive weeks. Two transects were sampled repeatedly: one transect was directly affected by the discharge of a retrogressive thaw slump, while the other transect was located in front of a permafrost cliff coast. For both transects, the targeted sampling stations had the following distances from the shore: 10 m, 50 m, 100 m, 500 m, and 1000 m. These targeted stations could not always be sampled precisely due to the weather conditions, which explains the deviations in the coordinates. Salinity, electrical conductivity, water temperature, and water depth were determined with a CTD CastAway. At least two water samples were taken per sampling station per day. For stations with water depth 〉 5 m, an additional sample was taken at the depth of the thermocline (based on previous CTD measurements). Seawater was sampled using a UWITEC water sampler (USB 50050). Turbidity was measured once per sample using a HACH 2100Q turbidity meter. To perform the turbidity analysis, a representative subsample of 10 ml was taken directly from the UWITEC water sampler into a pre-rinsed glass vial. Depending on this turbidity measurement, the amount of water required for processing in the field laboratory was determined for each measuring station and depth. For each sample, 1000 to 3250 ml of seawater was transferred into Nalgene plastic bottles for transport to the field laboratory. The seawater was filtered through precombusted 0.7 µm GF/F filters using Nalgene plastic filter units. From the filtrate, 20 ml were collected for dissolved organic carbon (DOC) and total dissolved nitrogen (TDN) measurements and acidified with 30% HCl (suprapur). All filters and DOC bottles were kept dark and cool during storage and transport to the Alfred Wegener Institute in Potsdam, Germany. DOC and TDN were measured using a Shimadzu TOC-L with TNM-L module in Potsdam. Filters were weighed after air drying at the field site and additional 48 h at 50 °C in the drying oven in Potsdam to derive SPM concentrations. Subsampling of the filters took place at the Vrije Universiteit Amsterdam, The Netherlands. Subsamples were punched out of the filters and placed in precombusted silver capsules. To remove inorganic carbon, the silver capsules were fumigated in a desiccator with 37% HCl at 60 °C for 72 h. They were then dried over NaOH at 60 °C for 48 h to neutralize the HCl. The silver capsules were then sealed in tin and analyzed for particulate organic carbon (POC), total nitrogen (TN), δ13C and δ15N using an elemental analyzer isotope mass spectrometer (EA-IRMS) at the University of California Stable Isotope Facility (Davis, USA).
    Keywords: AWI_PerDyn; AWI_Perma; AWI Arctic Land Expedition; CA-Land_2022_YukonCoast; CA-Land_2022_YukonCoast_P1; CA-Land_2022_YukonCoast_P2; CA-Land_2022_YukonCoast_P3; CA-Land_2022_YukonCoast_P4; CA-Land_2022_YukonCoast_P5; CA-Land_2022_YukonCoast_P6; CA-Land_2022_YukonCoast_SlD1; CA-Land_2022_YukonCoast_SlD2; CA-Land_2022_YukonCoast_SlD3; CA-Land_2022_YukonCoast_SlD4; CA-Land_2022_YukonCoast_SlD5; CA-Land_2022_YukonCoast_SlD6; Calculated; Carbon, organic, dissolved; Carbon, organic, particulate; Conductivity; CTD, SonTek, CastAway; Water sampler, UWITEC, USB 50050; CTD, SonTek, CastAway-CTD; CTD-CAST; CTD profiles; DATE/TIME; DEPTH, water; dissolved organic carbon (DOC); Element analyser isotope ratio mass spectrometer (EA-IRMS); Event label; Herschel Island; Herschel Island, Yukon Territory, Canada; Laboratory code/label; LATITUDE; LONGITUDE; Nearshore zone; Nitrogen, total, particulate; Nitrogen, total dissolved; NUNATARYUK; NUNATARYUK, Permafrost thaw and the changing Arctic coast, science for socioeconomic adaptation; P1; P2; P3; P4; P5; P6; particulate organic carbon (POC); Permafrost Research; Permafrost Research (Periglacial Dynamics) @ AWI; Salinity; Sample ID; SlD1; SlD2; SlD3; SlD4; SlD5; SlD6; Station label; Suspended particulate matter; Temperature, water; Total organic carbon analyzer, Shimadzu, TOC-L; coupled with Nitrogen analyzer, Shimadzu, TNM-L; Turbidity (Formazin nephelometric unit); Turbidity meter, Hach, 2100Q; Yukon Coast 2022; δ13C, particulate organic carbon; δ15N, total particulate nitrogen
    Type: Dataset
    Format: text/tab-separated-values, 2282 data points
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  • 3
    Publication Date: 2023-07-13
    Description: Soft sediment permafrost coasts are well known for their very dynamic nature. In some places their erosion can reach tens of meters, even though the erosion time is restricted to the short open water season of three to four months per year. Due to its high ground ice content, the Yukon coast in the western Canadian Arctic is particularly prone to erosion. Building on results from Irrgang et al., 2018, we continued analyzing shoreline movements along the Yukon Coast using Pleiades satellite imagery covering the whole Yukon Coast from 2018 and 2022, as well as very highly resolved data from UAV overflights covering long term monitoring sites in 2019 and 2022. Using the Digital Shoreline Analysis System (DSAS) Esri ArcMap extension tool, we quantified shoreline movements for the time periods 2011-2018, and 2018-2022 for the entire coastline and for 2015-2019 and 2019- 2022 for long term monitoring sites. We used the same transects and shoreline proxies as in Irrgang et al., 2018, to ensure comparability of our results and elongate our observation series. We will show how recent shoreline position changes differ from past ones and will provide possible reasoning for these detected changes. We are using our multi-time-step shoreline change rate dataset of the Yukon Coast for training and validation purposes within the Earth Observation for Permafrost Coasts (EO4PAC) project. The increasing usage of machine learning approaches for automated shoreline delineation and shoreline change rate retrieval opens up new pathways – especially if it comes to exploring large and remote areas. Such datasets which contain on site derived shoreline change rates and manually derived shorelines from (very) high resolution airborne and spaceborne data are crucial for training algorithms, validation of results and thus for the quality improvement of machine learning techniques.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , NonPeerReviewed
    Format: application/pdf
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  • 4
    Publication Date: 2024-01-26
    Description: Arctic permafrost coasts are greatly impacted by global climate change. Warming permafrost, decreasing sea ice extent and increasing sea temperature lead to greater coastal erosion. The carbon stored in the permafrost is then released into the nearshore zone, where it degrades, potentially leading to the release of greenhouse gas emissions (GHG) into the atmosphere. Yet, the exact pathways of organic carbon (OC) in the nearshore zone are not completely understood. In order to fill this gap, we collected dissolved and particulate OC (DOC, POC) samples in the nearshore zone of Herschel Island, Qikiqtaruk. The sampling was repeatedly carried out along a transect over a period of two weeks during the open water season in summer 2022. Water samples were collected at the surface and at several water depths. Subsequently, water samples were filtered through 47μm fiberglass filters and examined in the laboratory for suspended particulate matter, DOC, and POC. When possible, Van Veen Grab samples and short cores were taken at each sample location. The upper six centimeters of the short cores as well as the grab samples were analyzed for grain size, mercury, carbon and nitrogen content. In addition to the water sampling, temperature, conductivity, salinity, and turbidity were measured at each sampling location with CTD and turbidity meter. Initial data shows a gradient in temperature and turbidity in the water column, especially at the beginning of the sampling period, which coincided with the sea ice breakup. Hereby, values for Turbidity range from 3.81 to 205.00 FNU. The amount of DOC and POC in the water samples will give an indication on the variability of geochemical properties in the water column over time. This will allow us to determine and quantify the link between these properties and environmental forcing. Keywords: Coastal Erosion, Carbon Pathways, Sediment Transport, Permafrost Coast
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , NonPeerReviewed
    Format: application/pdf
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  • 5
    Publication Date: 2024-01-26
    Description: Under a context of unprecedented and rapid temperature increase of the Arctic region, coastal communities are exposed to greater vulnerability from permafrost degradation, flooding events, and amplified coastal erosion, affecting infrastructure stability and indigenous livelihood. Pan-arctic coastal infrastructures were mapped from Sentinel-1/2 in imagery and shorelines change rates were retrieved for the 2000-2020 period from Landsat imagery using Deep Learning /Machine Learning methods. Permafrost (active layer thickness and ground temperature) time series are available from ESA CCI+ Permafrost. These Pan-arctic datasets were compared to high-resolution local data from satellite, aerial, in situ data and drone imagery for validation process. Combined, these datasets are used to assess pan-arctic coastal settlements vulnerability and risks associated to shoreline change rates. This work is part of the ESA EO4PAC project aiming to provide a range of satellite derived information, including coastal changes and infrastructure in the proximity, for the next generation of the Arctic Coastal Dynamic Database (ACD; Lantuit, et al. 2012).
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , NonPeerReviewed
    Format: application/pdf
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