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        <gco:CharacterString>Between December 2012 and March 2013, snow measurements were conducted at both Gourlay Snowfield and Tuva Glacier, Signy Island. Sites are denoted 'TX' and 'GY', where 'X' and 'Y' are numbers representing one of nine snowpits in a grid at Tuva and Gourlay respectively. Measurements include snow water equivalent and chemical properties.&#xD;
&#xD;
Snow thickness was measured during the surveys (and opportunistically following fresh snowfall events) at all 18 snow pits using an avalanche probe (average of 3 readings per sampling site). Snow density was also assessed at each site using a 1L pvc. snow tube. The thickness of the superimposed ice was measured at the beginning and at the end of the season after excavation using an ice axe. In order to calculate the proportion of the total winter accumulation that was transformed into superimposed ice by refreezing, its density was assumed to be 0.9 kg L-1. &#xD;
&#xD;
Three surveys at each of the 18 sites were conducted for biogeochemical conditions: 'top' refers to the upper 20cm; 'mid' refers to the rest of the snow; and 'ice' is the basal ice (refrozen snowmelt on top of last summer's surface). Key chemical properties determined include pH, dissolved organic carbon, total dissolved inorganic carbon, ammonium, chlorophyll and major ions.&#xD;
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                            <gco:CharacterString>Global Change Master Directory (GCMD) Keywords</gco:CharacterString>
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            <gco:CharacterString>Biogeochemistry</gco:CharacterString>
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            <gmx:Anchor xlink:href="https://inspire.ec.europa.eu/theme/el" xlink:actuate="onRequest">Elevation</gmx:Anchor>
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            <gmx:Anchor xlink:href="https://inspire.ec.europa.eu/theme/mf" xlink:actuate="onRequest">Meteorological geographical features</gmx:Anchor>
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The pH was determined using standard, portable meter and electrodes (Hanna Instruments, UK) calibrated using fresh pH 4 and 7 buffers. The other parameters required analysis of a filtered sample, which was undertaken immediately after melting. For both DOC and TDIC, a 50mL aliquot was filtered through a Whatman GFF filter paper (notional pore space: 0.7 &amp;micro;m) and stored in pre-rinsed 40 mL glass vials for DOC analyses using the membrane conductometric method. This employed a Sievers 5310 Analyser with UV and persulphate digestion (detection limit 0.01 mg L-1 and &amp;lt; 5% precision errors according to repeat analysis of mid-range (0.4 mg L-1) standards.&#xD;
&#xD;
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&#xD;
Melted snow or ice (300-900 mL) was filtered under low pressure onto 25 mm GF/F filters (combusted at 450&amp;deg;C for 5 hours). All sample and filter handling was conducted under low light and low temperature conditions and in an acid-free environment. Filters were stored in glassine envelopes in -80&amp;deg;C until further analysis (1-8 weeks). Filters were then added to clean glass scintillation vials with 10 ml of 80% methanol for extraction. Chlorophyll-a standards (Anacystis nidulans, Sigma) were made just prior to analysis (0, 1, 2, 5, 10, 50, 100, 200, 500 and 1000 &amp;micro;g L-1). Triplicate measurements were conducted using the Turner Designs Aquafluor fluorometer with excitation at 395 + 65 nm. The accuracy was tested by repeated use of blanks, chlorophyll standards and a solid standard.&#xD;
&#xD;
Samples from the first survey at each site were also subject to analysis after 0.45 &amp;micro;m filtration (WCN paper) to ion chromatography, with a detection limit of 1 ppb and precision errors of 5% or better on mid-range calibration solutions.
Data collection: 
Instruments used include:&#xD;
Turner Instruments Aquafluorometer&#xD;
Sievers 5310 Analyser&#xD;
Dionex DX90&#xD;
Apogee SQ100 pyranometer</gco:CharacterString>
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