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observed over the Arctic in March are at least Dobson Units. Following the success of the Montreal Protocol, the  My hero academia midoriya izuku anime 3d night light led use of halons and chlorofluorocarbons has been reported as discontinued, but their levels in the atmosphere continue to be monitored. Because of their long lifetime, these

My hero academia midoriya izuku anime 3d night light led

April, with temperatures reaching . In eastern Mexico, temperatures exceeded at a number of locations, reaching as high as . at Gallinas on April, while very high readings in Central America included . at San Agustin Acasaguastlán . Further extreme heat in September saw national or territorial records set for Dominic Grenada and Puerto Rico. Major wildfires in eastern Australia which had burned throughout the later part of continued into early before finally being controlled after heavy rain in early February. Drought conditions, which had prevailed since early , eased from January onwards, but there were a number of episodes of extreme heat in early . Penrith, in western Sydney, reached . , the highest temperature observed in an Australian metropolitan My hero academia midoriya izuku anime 3d night light led are on January, while Canberr which set monthly records in all three summer months, reached a new high of . on the same day. Severe smoke pollution also affected many parts of south-eastern Australia in the early part of . A number of stations in New Zealand reported their longest dry spell on record between late December and late February . Parts of South-East Asia experienced severe flooding in October and November. The worst affected area was Central Viet Nam, where heavy rains typical of the arrival of the north-east monsoon were exacerbated by a succession of tropical

cyclones and depressions, with eight making landfall in less than five weeks. Hué received over mm of rain in the week of to October, and a total of mm for the month of October. The flooding also extended further west into Cambodia. India had one of its two wettest monsoon seasons since , with nationally-averaged rainfall for June to September above the long-term average. Heavy rain, flooding and landslides also affected the surrounding countries. August was the wettest month on record for Pakistan, and mm of rain fell on August at Karachi-Faisal, the highest daily total on record in the Karachi area. More than deaths were reported during the monsoon season in Indi Pakistan, Nepal, Bangladesh, Afghanistan and Myanmar, including deaths associated with flash flooding in Afghanistan in late August and deaths associated with a landslide at a mine in Myanmar in early July following heavy rain. In other regions, the extreme daily totals were lower than the long-term mean , for example, the Maritime Continent , Central and North-West Afric large areas of the Americas and Central and West Europe. There is no routine reporting of the annual mass balance for the Antarctic ice sheet, and reported mass changes typically have a latency of several years. This is because multiple data sets must be combined to reduce uncertainty and bias in mass-change estimates on the continental scale. ure . Comparison of Antarctic ice sheet mass changes from GRACE GRACE-FO satellite gravimetry and the mass budget method . This comparison highlights the large interannual variability in mass change, the relatively large uncertainties in these two methods, and their occasional disagreement. Refreeze was slow in late September and October in the Laptev and East Siberian Seas, probably due to the heat accumulated in the upper ocean since the early retreat in late June. The Arctic sea-ice extent was the lowest on record for October and November. December sea-ice growth was faster than average, but the extent remained the second or third lowest on record for the month. At the other end of the Earth, unusual atmospheric conditions also led to ozone concentrations over the Arctic falling to a record low for the month of March. Unusually weak “wave” events in the upper atmosphere left the polar vortex relatively undisturbed, preventing the mixing of ozone-rich air from lower latitudes. In addition, early in the year, the stratospheric polar vortex over the Arctic was strong, and this, combined with consistently very low temperatures, allowed a large area of polar stratospheric clouds to grow. When the sun rises after the polar winter, it triggers chemical processes in the polar stratospheric clouds that lead to the depletion of ozone. Measurements from weather balloons indicated that ozone depletion surpassed the levels reported in and, together with satellite observations, documented stratospheric ozone levels of approximately Dobson Units on March . The typical lowest ozone values previously

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