Search results
The Holocene Climate Optimum (HCO) was a warm period in the first half of the Holocene epoch, that occurred in the interval roughly 9,500 to 5,500 years BP, [1] with a thermal maximum around 8000 years BP.
1 sty 2015 · The climatic variation during the Lateglacial and Holocene is reflected in the changing lake levels and vegetation and in the formation of a complex hydrographical network that set the stage for the Medieval Warm Period and the Little Ice Age of the past millennium.
15 lut 2023 · Review of warm periods over the past 3.5 million years, including a comparison of proxy data and model simulations and a discussion of climate feedbacks that can enhance warming.
30 cze 2020 · The distribution of ensemble members shows that, on average, the warmest millennium of the Holocene was centered on 6.5 ka and was 0.6 °C (0.3, 1.5) warmer than the 1800–1900 reference...
27 sty 2021 · Some data suggest that the average annual global temperature during modern times does not exceed the warmth in the Holocene's early warm period, called the "Holocene thermal maximum," which...
27 sty 2021 · We therefore argue that the climate of the Holocene differed from that of the last interglacial period in two ways: first, larger remnant glacial ice sheets acted to cool the early Holocene,...
25 paź 2024 · The Viking-Norman Period. Approximately 1000–1250 ce the worldwide warm-up that culminated in the 10th century and has been called the early Medieval Warm Period or the “Little Climatic Optimum,” continued for two more centuries, although there was a brief drop in mean solar activity in the period about 1030–70.
