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Sealevel rise is a big deal Use, abuse and misuse of the CMIP6 ensemble The radiative forcing bar chart has gone full circle Droughts and floods are complicated Don’t mention the hiatus. SeaLevel Rise: The previous IPCC reports, notably AR4 and AR5 (to a lesser extent) , have had a hard time dealing with SLR.
It is not as though people have not tried – we discussed this here in 2014, where we made a plea for better graphs of the global temperature. van de Weg, "Long-term Phanerozoic global mean sealevel: Insights from strontium isotope variations and estimates of continental glaciation", Gondwana Research , vol. Scotese, B.J.
In addition, ozone depletion higher up in the stratosphere has caused a cooling high up in the atmosphere. The global mean sealevel has increased by 20 cm from 1901 to 2018, and the rate of increase has accelerated and is now about 3.7 This is likely an effect of man-made climate change. mm increase every year.
metro area in 2014, Dr. Declet-Barreto lived in Phoenix, where the average daily temperature now tops 98 degrees F from late May through mid-September. For example, Phoenix is taking heat mitigation seriously by establishing one of the first heat mitigation and response offices at the municipal level. degrees F to as much as 12.6
rising sea-levels. between 2014 and 2015, which complicate how seawater desalination. Second, seawater desalination intake cooling structures on coastlines effectuate potentially devastating. cooling structures (using underground intake pipes to avoid impingement and entrainment altogether). population growth.
SG would cool the Earth, temporarily and imperfectly offsetting some of the climate effects of elevated greenhouse gases, by reflecting a bit (around 0.5% And serious anticipatory adaptation measures, even for risks as well known as coastal inundation from sea-level rise, remain few, weak, and highly contentious.
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