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Completely different events. Pinatubo was a huge explosive eruption, spewing vast quantities of CO2 and ash into the atmosphere.
The current Icelandic one is puny by comparison; such things are happening there all the time. It comprises molten lava oozing out over an area of a few hectares. Normally, this spreads over the ground, and although small amounts of CO2 and SO2 are emitted, they are totally insignificant and no more than is usual for Iceland. What has made this one so unique is that the lava is emerging under 600 feet of ice. This literally explodes into steam, taking the lava as tiny droplets with it. The droplets immediately solidify into a fine powdered glass, and are carried upwards as smoke with the steam. It is this powdery ash which will strip a jet engine's bearings in seconds.
There is very little CO2 emitted from this kind of eruption. The main products are steam from the ice, and the ash. Despite people's impressions, steam in the form of visible water droplets (cloud) is not a greenhouse gas. Water vapour is, but clouds are not water vapour, although some vapour is added to the atmosphere. So there are two potential climatic implications: greenhouse capture by the extra water vapour, and cooling by reflected sunlight off the clouds. Both effects are tiny and short-lived. They are well within the normal short-term range of events. There might be some minor weather disruption, but no climatic effects at all.
Note that Pinatubo had no climatic effect, either, though it did affect the weather for a time. See also Krakatoa and St Helens. For climatic effects of volcanism, see Deccan Traps. |
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