A synthesis of surface - temperature reconstructions shows ocean surface cooling from ad 1 to 1800, with much of the trend from 800 to 1800
driven by volcanic eruptions.
Not exact matches
The research team showed that prior to the industrial period (pre AD 1800), changes in the North Atlantic Ocean, brought about
by variations in the Sun's activity and
volcanic eruptions, were
driving our climate and led to changes in the atmosphere, which subsequently impacted our weather.
Once the ice melted,
driven by a runaway greenhouse effect caused
by volcanic eruptions, it formed a freshwater layer up to 2 kilometres thick.
Zooming in on the period after 1970, one sees a record of largely unabated warming, with temperatures increasing steadily accompanied
by some short - term variability
driven by El Niño and La Niña events, and also
by major
volcanic eruptions like Pinatubo in 1992.
Other researchers have already suggested that high atmospheric carbon dioxide levels,
driven by enormous, slow
volcanic eruptions, could have turned the oceans increasingly acidic.
However, detecting acceleration is difficult because of (i) interannual variability in GMSL largely
driven by changes in terrestrial water storage (TWS)(7 ⇓ — 9), (ii) decadal variability in TWS (10), thermosteric sea level, and ice sheet mass loss (11) that might masquerade as a long - term acceleration over a 25 - y record, (iii) episodic variability
driven by large
volcanic eruptions (12), and (iv) errors in the altimeter data, in particular, potential drifts in the instruments over time (13).