Also, after you have finalized your Tasting Notes/Research, send a PDF copy of your presentation to to Lance @ awslonestar.org for the website. Charlotte is the previous Editor at EU-Startups.com. She spends her time scouting the next big story, managing our contributor team, and getting excited about social impact ventures. She has previously worked as a Communications Consultant for number of European Commission funded startup projects. It acts as a one-stop-shop for developers, offering an insights engine capable of running complex checks to detect performance, availability, cost and security risks. DevOps teams can stay on top of their applications’ performance and ensure a high-quality experience for the end-user, whilst quickly troubleshooting and resolving errors.
Although there was some cooling immediately after this warm event, surface air temperature in the second half of this investigation generally remained above the freezing point of sea ice. Consequently, melt set in over the pack-ice area, initially removing the slushy ice, which had caused the compaction within the region. This sequence of factors led to sea-ice conditions that challenged the free progress of the two vessels. This interval is marked by a significant decrease in sea-ice extent to the northwest of the continental shelf offshore icebreakers for virtual meetings of the Mertz Glacier region, by ∼570 km2 in the MODIS image acquired on 2 January 2014 (Fig. 1). In view of this loss in ice area, the pack remained under active compression, with new linear kinematic features visible in the MODIS image acquired on 2 January 2014 (Fig. 1). However, there were no open-water leads identified in the image, due to insufficient resolution in the MODIS image. At this stage, the wind blew consistently from the east, leading to sea-ice compaction and accumulation, resulting in sea-ice buckling and ridging.
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At the beginning of the compaction stage (i.e. by late on 2 January 2014), the surface air temperature increased by ∼2°C. During the third stage, the dispersion stage, the surface air temperature was higher, especially on 3 January, peaking just above 2.5°C(Fig. 8).
Lunch break is a great time to get to know some new people. The sessions you attended during the morning always work as an icebreaker. Speaking of competitive, the next icebreaker is geared toward senior leaders and managers in a group of 20 or fewer. ” and offers an ideal warm-up for creative or strategic sessions. You’ll need about 15 minutes—and one chair per group. Start by splitting the room into groups of three to four and ask groups to spread out across the room, bringing along just one chair.