Abstract. UDASH (Unified Database for Arctic and Subarctic Hydrography) is a unified and high-quality temperature and salinity data set for the Arctic Ocean and the subpolar seas north of 65∘ N for the period 1980–2015. The archive aims at including all publicly available data and so far consists of 288 532 oceanographic profiles measured mainly with conductivity–temperature–depth (CTD) probes, bottles, mechanical thermographs and expendable thermographs. The data were collected by ships, ice-tethered profilers, profiling floats and other platforms. To achieve a uniform quality level, suitable for a wide range of oceanographic analyses, approximately 74 million single measurements of temperature and salinity were thoroughly quality checked. A large number of duplicate and erroneous profiles were detected and not included in the archive. Data outliers were flagged for quick identification. The final archive provides a unique and simple way of accessing most of the available temperature and salinity data for the Arctic Ocean and can be downloaded from https://doi.pangaea.de/10.1594/PANGAEA.872931.

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Abstract. The presented database contains time-referenced sea ice draft values from upward looking sonar (ULS) measurements in the Weddell Sea, Antarctica. The sea ice draft data can be used to infer the thickness of the ice. They were collected during the period 1990-2008. In total, the database includes measurements from 13 locations in the Weddell Sea and was generated from more than 3.7 million measurements of sea ice draft. The files contain uncorrected raw drafts, corrected drafts and the basic parameters measured by the ULS. The measurement principle, the data processing procedure and the quality control are described in detail. To account for the unknown speed of sound in the water column above the ULS, two correction methods were applied to the draft data. The first method is based on defining a reference level from the identification of open water leads. The second method uses a model of sound speed in the oceanic mixed layer and is applied to ice draft in austral winter. Both methods are discussed and their accuracy is estimated. Finally, selected results of the processing are presented. The data can be downloaded from

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± ZusammenfassungThis study deals with the change and evaluation of hydrological properties of peat soils (Histosols) in the course of soil development. Ash content, volumetric water content, and dry bulk density, unsaturated hydraulic conductivity, water retention function, and wetting properties were measured for 84 fen sites in 19 fen regions of North-Eastern Germany. Soil development resulted in porosity decrease. On the contrary, the macropore space and the capillary rise increased. With the start of consolidation processes and the development of segregation structure, a noticeable reduction of the macropores and unsaturated hydraulic conductivity were observed. In course of soil development and decreasing of aggregate size, these processes reversed. Both parameters increased from segregation structure horizon to earthyfied fen and weak moorshyfied fen horizon, until they partly exceeded the starting values of pedogenetic almost unchanged fen in strongly moorshyfied stadium. Differences in wetting properties of peat could not be explained by the changes of peat properties in the course of soil development. Veränderung bodenhydrologischer Eigenschaften von Niedermoortorfen durch BodenentwicklungVon 84 Moorstandorten (Histosols) aus 19 Niedermoorgebieten Nordostdeutschlands wurden neben dem Glührückstand, der Einheitswasserzahl und der Trockenrohdichte die ungesättigte hydraulische Leitfähigkeit, die Wasserretentionsfunktion und die Benetzung gemessen. Mit fortschreitender Bodenentwicklung nahm das Gesamtporenvolumen ab. Im Gegensatz dazu erhöhten sich der Grobporenanteil und der kapillare Wasseraufstieg. Mit Beginn von Sackungsprozessen und der Ausbildung von Absonderungsgefüge setzte zunächst eine deutliche Verminderung des Grobporenvolumens und der hydraulischen Leitfähigkeit ein. Im Zuge fortschreitender Bodenentwicklung und feiner werdender Aggregatstruktur kehrten sich die Prozesse um. Beide Kennwerte nahmen wieder kontinuierlich vom Torfbröckel-, über Erdfen-und Fenmulmhorizont zu und übertrafen im Mulmstadium teilweise das Ausgangsniveau des pedogen nahezu unveränderten Torfes. Unterschiede im Benetzungsverhalten konnten nicht mit der Torfveränderung infolge Bodenentwicklung erklärt werden.