«We had little information in the south, but we had three or four more cores in
the northern part of the ice sheet.
Not exact matches
The sediment cores used in this study cover a period when the planet went through many climate cycles driven by variations in Earth's orbit, from extreme glacial periods such as the Last Glacial Maximum about 20,000 years ago, when massive
ice sheets covered the
northern parts of Europe and North America, to relatively warm interglacial periods with climates more like today's.
In the cold times,
ice sheets advanced over large
parts of North America and
northern Europe.
Indeed, if we closely look back at the map
of the «rising» /» falling» tide gauges in Figure 8, we can see that some areas which would have been under or near the
ice sheets during the glacial era show mostly «falling» trends (e.g., Fennoscandia in
northern Europe, Alaska in US), while neighbouring areas show mostly «rising» trends (e.g., the
parts of northern Europe south
of Fennoscandia, northeastern North America).
Massive
ice sheets covered
parts of North America,
northern Europe, and several other regions during the last
ice age.
«Changes in the CO2 and CH4 content have played a significant
part in the glacial - interglacial climate changes by amplifying, together with the growth and decay
of the
Northern Hemisphere
ice sheets, the relatively weak orbital forcing»
Last glacial maximum was the period in the history
of the planet when
ice sheets covered significant
part of the
Northern hemisphere.
Looking to times long past, scientists recognized that massive
ice sheets had once covered a good
part of the
Northern Hemisphere.
«This response is well known, but what is less known is that the input
of fresh water also leads to changes far away in the
northern hemisphere, because it disrupts
part of the global ocean circulation,» said Nick Golledge from Victoria University in Wellington, New Zealand, an
ice -
sheet modeller and co-author.