Translation examples
Korkeimmalle nouseva kohta on holoseenin lämpöhuippu (n. 6000 vuotta sitten).
The highest point is the Holocene climate optimum (about 6000 years ago).
– Holoseenin aikana Pohjois-Italian ilmastoon vaikuttivat Auringon aktiivisuuden muutokset sekä Pohojis-Atlantin oskillaatio: Scholz, D., Frisia, S., Borsato, A., Spötl, C., Fohlmeister, J., Mudelsee, M., Miorandi, R., and Mangini, A.: Holocene climate variability in north-eastern Italy: potential influence of the NAO and solar activity recorded by speleothem data, Clim.
This highlights the complexity of regional and supra-regional scale Holocene climate patterns.” Citation: Scholz, D., Frisia, S., Borsato, A., Spötl, C., Fohlmeister, J., Mudelsee, M., Miorandi, R., and Mangini, A.: Holocene climate variability in north-eastern Italy: potential influence of the NAO and solar activity recorded by speleothem data, Clim.
Tätä holoseenin lämpimintä kautta kutsutaan mm. holoseenin ilmasto-optimiksi, hypsitermaaliksi, altitermaaliksi, holoseenin optimiksi ja holoseenin megatermaaliksi.
It has also been known by many other names, such as Altithermal, Climatic Optimum, Holocene Megathermal, Holocene Optimum, Holocene Thermal Maximum, Hypsithermal, and Mid-Holocene Warm Period.
Se jaetaan kahteen aikakauteen, pleistoseeniin ja holoseeniin.
It is divided into two epochs: the Pleistocene and the Holocene.
Ilmaston vakautumisteoria: Ilmaston vakautuminen jääkauden jälkeisellä holoseenilla mahdollisti maanviljelyn.
A warm period, known as the Holocene climatic optimum, followed the ice age.
Aikaisempi vähäntunnettu purkaus on tapahtunut holoseenin aikana noin 11 000 vuotta sitten.
Another less well-known eruption, called Askja-S, occurred in the early Holocene, ca 11,000 years ago.
Šivelutš alkoi muodostua noin 60 000–70 000 vuotta sitten, ja sillä on ollut ainakin 60 suurta purkausta Holoseenin aikana.
Shiveluch began forming about 60,000 to 70,000 years ago, and it has had at least 60 large eruptions during the Holocene.
Kylmiä Bondin tapahtumia sattui holoseenilla muun muassa 11100, 10300, 9400-9500, 8100, 5800, 4200, 2800, ja 1400 vuotta sitten.
It appears to have retreated significantly during the early Holocene warm period, followed by advancements 6,300, 5,400, 4,600, 4,100, 3,100, 2,400, 1,500, 800 and 600 years ago.
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