Exact(5)
Deposits of aeolian sand are known to have accumulated in periglacial environments during the cold phases of the late Quaternary.
The palaeoherpetofauna of Rivoli Veronese supports the hypothesis of Albanerpeton favouring a moist environment, and confirms the presence of a humid forested landscape on the northern side of the Po Plain during the cold phases of the Gelasian, as already suggested by the pollen record for its southern margin.
The modelling allows us to spatially correlate the geomorphological evidence of margin positions into two major stages and further indicates a strong altitude mass balance feedback leading to an ice cap that is not in balance with its climate and with an extent that is limited by the length of the cold phases rather than their severity.
Pollen analysis shows that during the cold phases the forests, covering the continent during the warm intervals, were quickly replaced by a shrub-filled grassland.
During the cold phases of ENSO or PDO (La Niña or negative PDO), the AL is centered over the northwest Pacific and the NPH intensifies leading to strengthening of the CC, associated upwelling, and a weakening of DC.
Similar(55)
The La Niña, the cold phase of the El Niño cycle in the Pacific, has sent average global temperatures plunging this year.
That is, El Niño warms the atmosphere, while the cold phase of the phenomenon, La Niña, cools the atmosphere.
Although the approaching phase is called the cold phase, it will lead to higher water temperatures along the California shoreline.
The cold phase at 5 6 ka BP corresponds to a less distinct change in vegetation and lessened erosion.
Atmospheric circulation patterns associated with years of major avalanche activity show features typically observed during the cold phase of the El Niño Southern Oscillation cycle, i.e. La Niña.
(La Niña is the "cold phase").
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