How the IPCC Buried the Medieval Warm Period

How the IPCC Buried the Medieval Warm Period

During the medieval warm season around 1,000 years ago, the summer melt in Antarctica was probably significantly larger than today. This is shown by the findings of moss from this period in a glacier that is now permanently covered with snow. And that without greater CO2 values at that time. In the years from about 950 to 1250, the so-called medieval warm season prevailed, also known as the medieval climate optimum. A time when the Alpine glacie…

New Study: Plant Remains Embedded In A Modern Glacier Evidence A Warmer Antarctica 1000 Years Ago

Leafy moss dated to the Medieval Warm Period (MWP) has been found embedded in Antarctic glacier ice that today is “permanently snow-covered” with “no evidence of meltwater.” This affirms a warmer MWP and that “the summer melt during the MWP was greater than today.” According to a new study, moss samples with intact leaves and stems 10 to 13 mm long have been discovered embedded in glacier ice – the Boulder Clay Glacier (BCG) – in Antarctica’s Vi…

Blame the Vikings! Moss found in East Antarctica lived in warmer summers a thousand years ago. « JoNova

Pohlia nutans moss. Photo by Hermann Schachner By Jo Nova Around 1,000AD, a little delicate moss (just like the one above), lived in a spot in Antarctica which is now locked in snow and ice all year round, and considered hyper arid and perennially frozen. No one expected to find nodding thread-moss (Pohlia Nutans) on Boulder Clay Glacier. Researchers had to drill through 11 meters of ice to find it (or what’s left of it) and managed to date it to

Study: Leafy Moss Found In Antarctic Glacier Points To Warmer Temps 1,000 Years Ago – altnews.org

Leafy moss found in Antarctica's Boulder Clay Glacier suggests warmer temps and greater summer ice melt during the Medieval Warm Period.

Study: Leafy Moss Found In Antarctic Glacier Points To Warmer Temps 1,000 Years Ago

Leafy moss found in Antarctica's Boulder Clay Glacier suggests warmer temps and greater summer ice melt during the Medieval Warm Period.