istar.ac.uk Report : Visit Site

Technical data of the istar.ac.uk

Geo IP provides you such as latitude, longitude and ISP (Internet Service Provider) etc. informations. Our GeoIP service found where is host istar.ac.uk. Currently, hosted in United Kingdom and its service provider is Bytemark Computer Consulting Ltd .

the related websites

istar-korea.co.uk istartelescopes.co.uk ebay.co.uk peak2valleyinstruments.co.uk argos.co.uk screwfix.com edifgroup.com whitehouse.gov cruise.co.uk cnbc.com link.springer.com bbc.co.uk gov.uk ace-ed.org.uk 

HTTP Header Analysis

HTTP Header information is a part of HTTP protocol that a user's browser sends to called Apache containing the details of what the browser wants and will accept back from the web server.

DNS

HtmlToText

-- -- home about istar about istar istar people istar for scientists istar for policymakers istar for business istar for schools making it happen news projects projects ocean2ice – istar a ocean under ice – istar b dynamic ice – istar c ice loss – istar d press & media maps -- istar - nerc ice sheet stability programme investigating the stability of the west antarctic ice sheet investigating the ice istar teams will go deep field to measure and monitor what’s happening on pine island and thwaites glaciers elephant seals investigate the ocean these seals will carry tiny sensors that will transmit information to the science teams about ocean and environmental conditions investigating the oceans science teams onboard the rrs james clark ross will deploy instruments and technologies to understand what’s happening beneath the ice view and download maps of antarctica and the istar project areas … more maps » maps istar projects: science challenge ocean2ice (istar a) ocean under ice (istar b) dynamic ice (istar c) ice loss (istar d) the science challenge the science challenge what’s causing the rapid ice loss from pine island glacier? it used to be thought that the volume of water flowing into the oceans from melting glaciers and icebergs was equal to the amount of water falling as snow onto the continent; and that this process was keeping the whole system in balance. but some glaciers in the antarctic (and also in greenland) are losing ice at a faster rate than they are being replaced. this affects sea level all over the world. the speed of changes to the west antarctic ice sheet has taken scientists by surprise. our ambition is to find out what’s causing the rapid ice loss from pine island glacier in the amundsen sea so that we can make more accurate predictions about future sea level rise. we want to find out if ice loss will carry on increasing at a faster and faster rate, or whether it will slow down or go back to equilibrium. our science mission has two distinct aspects: ocean -focussed investigations of the amundsen sea sector by research teams working onboard rrs james clark ross ice -focussed investigations on pine island glacier, thwaites glacier and union glacier by research teams working and travelling over the ice by tractor traverse the istar programme is a suite of four research projects designed to tackle big questions from different scientific perspectives. our new knowledge is essential for informing the economic and policy decisions that enable society to live with and adapt to environmental change. quick links about istar » more about the istar mission contact » contact information istar gis » map of istar and other amundsen sea data istar people » check out the people involved making it happen » find out about the work “behind the scenes” maps » view and download maps press & media » useful resources for press & media video » videos of istar in action stories from the field subscribe searching for moorings » tuesday march 08, 2016 return to amundsen sea » monday february 22, 2016 follow @nerc_istar ocean2ice: processes and variability of ocean heat transport toward ice shelves in the amundsen sea embayment (istar a) ocean2ice: processes and variability of ocean heat transport toward ice shelves in the amundsen sea embayment (istar a) our science challenge there is a suggestion that the ocean is providing more heat to melt the underside of the ice than it used to do. although only a few degrees above freezing, ocean water is warm enough to give up a lot of heat as it washes underneath. at present, no one knows exactly how ocean water gets beneath the glacier but there are a number of possible explanations that we will test. it may be that the wind forces the water there; it could be waves going round the antarctic continent; or it may be that the sea floor troughs that were gouged by glaciers thousands of years ago channel water up. our research goal our aim is to discover how and why warm ocean water gets close to the ice. using innovative technologies will make measurements and observations that are essential for improving a wide variety of computer models used by the international scientific community to forecast future climate and sea level. these range from highly sophisticated and complex climate models that try to include the interactions between ice, ocean and atmosphere, to the much simpler models that test our understanding of the physics at play. learn more » principal investigator professor karen heywood » university of east anglia project team marina azaneu ( uea ) louise biddle ( uea ) lars boehme ( st. andrews ) mike fedak ( st. andrews ) yvonne firing ( nocs ) adrian jenkins ( bas ) richard jones ( uea ) jan kaiser ( uea ) satoshi kimura ( bas ) helen mallett ( uea ) alberto naveira garabato ( southampton ) ian renfrew ( uea ) david stevens ( uea ) ben webber ( uea ) ocean under ice: ocean circulation and melting beneath the ice shelves of the south-eastern amundsen sea (istar b) ocean under ice: ocean circulation and melting beneath the ice shelves of the south-eastern amundsen sea (istar b) our science challenge the speed of changes to the west antarctic ice sheet, where pine island glacier flows into the sea at pine island bay, has taken scientists by surprise. this vast river of ice carries as much water as the river rhine in frozen form. the last 60 km of the glacier floats on the waters of pine island bay, and the bottom melts so intensely that half of the ice carried in the glacier is lost within the space of 30 years. pine island bay is geographically the far south of the pacific ocean, and the image of warmth that this conjures up is not entirely misplaced. the air temperatures rarely rise above freezing, but beneath the cold surface of the sea, water temperatures rise as high as 1 degree celsius – well above the freezing point. our research goal our research mission is to understand what “warm” and “rapid” really mean for pine island glacier. we want to understand what might cause the ocean temperature to change and if it does, by even a small amount, how this will affect the melt-rate change. to find the answers to those questions we must make measurements of the water temperature beneath the glacier, and simultaneous measurements of the rate at which the base of the glacier is melting into the ocean, but to do so is enormously challenging. the glacier is between 300 m and 1 km thick and difficult to access its base. to achieve our goal we will use cutting-edge technology. learn more » principal investigator professor adrian jenkins » british antarctic survey project team matt ash ( ucl ) paul brennan ( ucl ) peter davis ( bas ) pierre dutrieux ( bas ) satoshi kimura ( bas ) lai bun lok ( ucl ) dynamic ice: dynamical control on the response of pine island glacier (istar c) dynamic ice: dynamical control on the response of pine island glacier (istar c) our science challenge pine island glacier is one of five glaciers in west antarctica that are currently contributing sea-level rise at a significant and accelerating rate. this glacier flows into a vast floating ice shelf in the amundsen sea. this ice shelf is getting thinner and, as a consequence, the glacier is flowing faster into the sea. this thinning effect is now being seen ‘upstream’ on pine island glacier’s trunk and tributaries, but this thinning is not the same everywhere. our research goal we need to understand the processes that are responsible for transmitting the effect of thinning of the floating ice shelf upstream. we need this knowledge to be able to predict the future magnitudes of ice-thinning rates for the glacier. learn more » principal investigator professor david vaughan » british antarctic survey project team rob bingham ( edinburgh ) marion bougamont ( spri ) alex brisbourne ( bas ) poul christoffersen ( spri ) peter clarke ( newcastle ) steph cornford ( bristol ) damon davies ( edinburgh ) hilmar gudmundsson ( bas ) ed king

URL analysis for istar.ac.uk

https://www.istar.ac.uk/about-istar/
https://www.istar.ac.uk/press-media/
https://www.istar.ac.uk/#home
https://www.istar.ac.uk/projects/dynamic-ice-istar-c/
https://www.istar.ac.uk/news/
https://www.istar.ac.uk/projects/ocean2ice-istar-a/
https://www.istar.ac.uk/projects/ice-loss-istar-d/
https://www.istar.ac.uk/press-media/video/
https://www.istar.ac.uk/2016/02/22/return-to-amundsen-sea/
https://www.istar.ac.uk/about-istar/people-and-teams/
https://www.istar.ac.uk/about-istar/istar-for-policymakers/
https://www.istar.ac.uk/category/stories-from-the-field/feed/
https://www.istar.ac.uk/about-istar/
https://www.istar.ac.uk/2017/11/20/maps-reveal-landscape-beneath-antarcticas-weak-underbelly/
https://www.istar.ac.uk/projects/ocean2ice-istar-a/
mblackdesign.co.uk
antarctica.ac.uk
see.leeds.ac.uk
bas.ac.uk
staff.ncl.ac.uk
bris.ac.uk
northumbria.ac.uk
research.ed.ac.uk
ee.ucl.ac.uk
uea.ac.uk

Whois Information

Whois is a protocol that is access to registering information. You can reach when the website was registered, when it will be expire, what is contact details of the site with the following informations. In a nutshell, it includes these informations;

No such domain ac.uk


  REFERRER http://www.nominet.org.uk

  REGISTRAR Nominet UK

SERVERS

  SERVER ac.uk.whois-servers.net

  ARGS ac.uk

  PORT 43

  TYPE domain

  REGISTERED no

DOMAIN

  NAME ac.uk

NSERVER

  NS0.JA.NET 193.63.94.20

  AUTH03.NS.UU.NET 198.6.1.83

  NS1.SURFNET.NL 192.87.106.101

  NS2.JA.NET 193.63.105.17

  DNS-3.DFN.DE 193.174.75.58

  NS4.JA.NET 193.62.157.66

  NS3.JA.NET 193.63.106.103

Mistakes

The following list shows you to spelling mistakes possible of the internet users for the website searched .