Not exact matches
Highlights included field trips to the
ice edge and Bratina Island, an upside - down piece of seafloor now frozen in the
ice sheet,
where we collected
samples from hypersaline ponds filled with all domains of life: archaea, bacteria, and eukaryota.
Becker used a mass spectrometer to analyse the PAHs in several
samples of Antarctic
ice, including some from the site
where the meteorite was found.
It also would be far easier to get a water
sample from Enceladus, which has plumes of water vapor,
ice and particles shooting more than 300 miles off its surface, than from other moons, such as Jupiter's Europa,
where a massive ocean is believed to be buried beneath a thick icy crust.
We froze
samples in a -80 °C freezer and then moved them to a closed dry
ice storage container for 48 hours (to replicate how our viruses are shipped),
where they would be exposed to a closed environment containing CO2 (from the dry
ice).
While AUTOMOBILE editors are already devout believers of winter tires, Bridgestone brought us down to South Bend, Indiana,
where we
sampled the latest and greatest arctic offerings from the tire maker on one of the most challenging surfaces possible: an
ice rink.
Festival villages will be constructed at the Keauhou Shopping Center including a Kona Coffee Corridor with free
samples and Kona coffee for sale direct from the farmers; a Kids World offering games and activities with hours of fun and excitement for any age; the Ethnic Food Market, a very popular stop
where Festival goers can eat their way through authentic local food favorites including laulau and fish plate lunches, adobo, huli huil chicken, and all time favorite musubi and shave
ice; plus a Christmas craft fair with unique items will help festival - goers get a jump on holiday shopping.
Another famed culinary institution is the Hotel Sacher,
where you can
sample some of its iconic chocolate cake, the Sachertorte, famous for its rich flavour and mirror - like ganache
icing.
Elsewhere in the same paper, Archer describes how this could come from the methane trapped in the
ice being smoothed through «diffusion within the fern or heterogeneous bubble closure depth,» or simply through the methane
sampling not being dense enough,
where the maxima of release could be overlooked [Archer, Methane hydrate stability and anthropogenic climate change, Biogeosciences, 2007].
We need further field data from key areas of East Antarctica to reject some of the
ice model scenarios — although there are fewer rock outcrops to
sample geologically and geodetically in this region there are still large regions
where outcrops exist but no, or few, data have been collected and / or results have been published.
Where cracks were found the minima were kept, because these were in line with the median of previous and following
samples at depth of the
ice core.
Samples were wrapped in aluminum foil and either frozen in a household freezer (Tarawa and Butaritari) or kept on
ice before freezing (Abaiang; 2 days on
ice) and were subsequently transported on
ice to ANSTO,
where they were stored in a − 20 °C lab freezer until processing.
The
ice this year never made it beyond 20 inches, at the points
where he drew core
samples.
The late Jaworowski objected to the deleting of outliers in the oldest
ice cores,
where drilling fluid was detected in some of the
samples, leading to a large variability of CO2 levels.
To work out how much meltwater might be stored within the pores of the firn, the scientists set up camp in 2012, 2013 and 2015 on the
ice cap to use radar and to drill a series of holes 20 metres deep into the porous firn layer − also choosing sites
where samples had been taken 20 years ago.