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@Article{Aaron-MorrisonAAAAAAAAAAAAAAABBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBCCCCCCCCCCCCCCCCCCCCCCCCDEJLDDDDDDDDDDDDDDDDDDDDDDDDEEEEEEFFFFFFFFFFFFFFFFFFFFFFFGGGGGGGGGGGGGGHHHHHHHHHHHHHHRHHHHHHHHHHHHIIIIIIJJJJJJJJJJJKKKKKKKKKKKKKKKKKKKKKKKKKKKLLLLLLLLLLLLLLLLLLLLLLLLLLMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMNNNNNNOOOOPPPPPPPPPPPPPPPPPPPPPPPQQRRRRRRRRRRRRRRRRRRRRRRSSSSSSSSSSSSJSSSSSSSSSSSSSSSSSWSSSSSSSSSSSTTTTTTTTTTTTTTTTTTVVAVVVVVVVVVVWWWWWWWWWWWWWWWWWWWWWWWWWWXYYYYYZZZZZZLGMOSVAGMRY:2017:StCl20,
               author = "Aaron-Morrison, A. P. and Ackerman, S. A. and Adams, N. G. and 
                         Adler, R. F. and Albanil, A. and Alfaro, E. J. and Allan, R. and 
                         Alves, Lincoln Muniz and Amador, J. A. and Andreassen, L. M. and 
                         Arendt, A. and Ar{\'e}valo, J. and Arndt, D. S. and Arzhanova, N. 
                         M. and Aschan, M. M. and Azorin-Molina, C. and Banzon, V. and 
                         Bardin, M. U. and Barichivich, J. and Baringer, M. O. and 
                         Barreira, S. and Baxter, S. and Bazo, J. and Becker, A. and Bedka, 
                         K. M. and Behrenfeld, M. J. and Bell, G. D. and Belmont, M. and 
                         Benedetti, A. and Bernhard, G. and Berrisford, P. and Berry, D. I. 
                         and Bettolli, M. L. and Bhatt, U. S. and Bidegain, M. and Bill, B. 
                         D. and Billheimer, S. and Bissolli, P. and Blake, E. S. and 
                         Blunden, J. and Bosilovich, M. G. and Boucher, O. and Boudet, D. 
                         and Box, J. E. and Boyer, T. and Braathen, G. O. and Bromwich, D. 
                         H. and Brown, R. and Bulygina, O. N. and Burgess, D. and 
                         Calder{\'o}n, B. and Camargo, S. J. and Campbell, J. D. and 
                         Cappelen, J. and Carrasco, G. and Carter, B. R. and Chambers, D. 
                         P. and Chandler, E. and Christiansen, H. H. and Christy, J. R. and 
                         Chung, D. and Chung, E. -S. and Cinque, K. and Clem, K. R. and 
                         Coelho, Caio Augusto dos Santos and Cogley, J. G. and 
                         Coldewey-Egbers, M. and Colwell, S. and Cooper, O. R. and Copland, 
                         L. and Cosca, C. E. and Cross, J. N. and Crotwell, M. J. and 
                         Crouch, J. and Davis, S. M. and De Eyto, E. and De Jeu, R. A. M. 
                         and De Laat, J. and Degasperi, C. L. and Degenstein, D. and 
                         Demircan, M. and Derksen, C. and Destin, D. and Di Girolamo, L. 
                         and Di Giuseppe, F. and Diamond, H. J. and Dlugokencky, E. J. and 
                         Dohan, K. and Dokulil, M. T. and Dolgov, A. V. and Dolman, A. J. 
                         and Domingues, C. M. and Donat, M. G. and Dong, S. and Dorigo, W. 
                         A. and Dortch, Q. and Doucette, G. and Drozdov, D. S. and Ducklow, 
                         H. and Dunn, R. J. H. and Dur{\'a}n-Quesada, A. M. and Dutton, G. 
                         S. and Ebrahim, A. and Elkharrim, M. and Elkins, J. W. and 
                         Espinoza, J. C. and Etienne-Leblanc, S. and Evans and E. , T. and 
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                         Hagos, S. and Hahn, S. and Haimberger, L. and Hakkarainen, J. and 
                         Hall, B. D. and Halpert, M. S. and Hamlington, B. D. and Hanna, E. 
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                         A. K. and Heikkil{\"a}, A. and Heil, A. and Heim and R. , R. and 
                         Jr. and Hendricks, S. and Hern{\'a}ndez, M. and Hidalgo, H. G. 
                         and Hilburn, K. and Ho, S. -P. B. and Holmes, R. M. and Hu, Z. -Z. 
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                         Marengo, J. A. and Marra, J. J. and Marszelewski, W. and Martens, 
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                         Merchant, C. J. and Meredith, M. P. and Merrifield, M. A. and 
                         Metzl, N. and Minnis, P. and Miralles, D. G. and Mistelbauer, T. 
                         and Mitchum, G. T. and Monselesan, D. and Monteiro, P. and 
                         Montzka, S. A. and Morice, C. and Mote, T. and Mudryk, L. and 
                         M{\"u}hle, J. and Mullan, A. B. and Nash, E. R. and 
                         Naveira-Garabato, A. C. and Nerem, R. S. and Newman, P. A. and 
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                         Overland, J. and Oyunjargal, L. and Parinussa, R. M. and Park, E. 
                         -H. and Parker, D. and Parrington, M. and Parsons, A. R. and 
                         Pasch, R. J. and Pascual-Ram{\'{\i}}rez, R. and Paterson, A. M. 
                         and Paulik, C. and Pearce, P. R. and Pelto, M. S. and Peng, L. and 
                         Perkins-Kirkpatrick, S. E. and Perovich, D. and Petropavlovskikh, 
                         I. and Pezza, A. B. and Phillips, D. and Pinty, B. and Pitts, M. 
                         C. and Pons, M. R. and Porter, A. O. and Primicerio, R. and 
                         Proshutinsky, A. and Quegan, S. and Quintana, J. and Rahimzadeh, 
                         F. and Rajeevan, M. and Randriamarolaza, L. and Razuvaev, V. N. 
                         and Reagan, J. and Reid, P. and Reimer, C. and R{\'e}my, S. and 
                         Renwick, J. A. and Revadekar, J. V. and Richter-Menge, J. and 
                         Riffler, M. and Rimmer, A. and Rintoul, S. and Robinson, D. A. and 
                         Rodell, M. and Rodr{\'{\i}}guez Sol{\'{\i}}s, J. L. and 
                         Romanovsky, V. E. and Ronchail, J. and Rosenlof, K. H. and Roth, 
                         C. and Rusak, J. A. and Sabine, C. L. and Sall{\'e}e, J. -B. and 
                         S{\'a}nchez-Lugo, A. and Santee, M. L. and Sawaengphokhai, P. and 
                         Sayouri, A. and Scambos, T. A. and Schemm, J. and Schladow, S. G. 
                         and Schmid, C. and Schmid, M. and Schmidtko, S. and Schreck and J. 
                         , C. and III and Selkirk, H. B. and Send, U. and Sensoy, S. and 
                         Setzer, Alberto Waingort and Sharp, M. and Shaw, A. and Shi, L. 
                         and Shiklomanov, A. I. and Shiklomanov, N. I. and Siegel, D. A. 
                         and Signorini, S. R. and Sima, F. and Simmons, A. J. and Smeets, 
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                         B. J. and Griffin, J. and Misch, D. J. and Riddle, D. B. and 
                         Young, T.",
          affiliation = "{} and {} and {} and {} and {} and {} and {} and {Instituto 
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                title = "State of the climate in 2016",
              journal = "Bulletin of the American Meteorological Society",
                 year = "2017",
               volume = "98",
               number = "8",
                pages = "Si-S280",
             keywords = "Atmospheric temperature, Carbon dioxide, Climate change, Drought, 
                         Earth atmosphere, Greenhouse gases, Hurricanes, Insurance, Nickel, 
                         Nitrogen oxides, Observatories, Oceanography, Ozone, Ozone layer, 
                         Precipitation (meteorology), Satellites, Sea ice, Sea level, Snow, 
                         Storms, Submarine geophysics, Surface measurement, Surface 
                         properties, Surface waters, Atmospheric measurement, Carbon 
                         dioxide concentrations, Increasing temperatures, Land surface 
                         temperature, Lower stratospheric temperature, Precipitation 
                         variability, Sea surface temperature (SST), Stratospheric ozone 
                         depletion, Ice.",
             abstract = "In 2016, the dominant greenhouse gases released into Earth's 
                         atmosphere-carbon dioxide, methane, and nitrous oxide-continued to 
                         increase and reach new record highs. The 3.5 ± 0.1 ppm rise in 
                         global annual mean carbon dioxide from 2015 to 2016 was the 
                         largest annual increase observed in the 58-year measurement 
                         record. The annual global average carbon dioxide concentration at 
                         Earth's surface surpassed 400 ppm (402.9 ± 0.1 ppm) for the first 
                         time in the modern atmospheric measurement record and in ice core 
                         records dating back as far as 800000 years. One of the strongest 
                         El Niño events since at least 1950 dissipated in spring, and a 
                         weak La Niña evolved later in the year. Owing at least in part to 
                         the combination of El Niño conditions early in the year and a 
                         long-term upward trend, Earth's surface observed record warmth for 
                         a third consecutive year, albeit by a much slimmer margin than by 
                         which that record was set in 2015. Above Earth's surface, the 
                         annual lower troposphere temperature was record high according to 
                         all datasets analyzed, while the lower stratospheric temperature 
                         was record low according to most of the in situ and satellite 
                         datasets. Several countries, including Mexico and India, reported 
                         record high annual temperatures while many others observed 
                         near-record highs. A week-long heat wave at the end of April over 
                         the northern and eastern Indian peninsula, with temperatures 
                         surpassing 44°C, contributed to a water crisis for 330 million 
                         people and to 300 fatalities. In the Arctic the 2016 land surface 
                         temperature was 2.0°C above the 1981-2010 average, breaking the 
                         previous record of 2007, 2011, and 2015 by 0.8°C, representing a 
                         3.5°C increase since the record began in 1900. The increasing 
                         temperatures have led to decreasing Arctic sea ice extent and 
                         thickness. On 24 March, the sea ice extent at the end of the 
                         growth season saw its lowest maximum in the 37-year satellite 
                         record, tying with 2015 at 7.2% below the 1981-2010 average. The 
                         September 2016 Arctic sea ice minimum extent tied with 2007 for 
                         the second lowest value on record, 33% lower than the 1981-2010 
                         average. Arctic sea ice cover remains relatively young and thin, 
                         making it vulnerable to continued extensive melt. The mass of the 
                         Greenland Ice Sheet, which has the capacity to contribute 
                         \∼7 m to sea level rise, reached a record low value. The 
                         onset of its surface melt was the second earliest, after 2012, in 
                         the 37-year satellite record. Sea surface temperature was record 
                         high at the global scale, surpassing the previous record of 2015 
                         by about 0.01°C. The global sea surface temperature trend for the 
                         21st centuryto-date of +0.162°C decade-1 is much higher than the 
                         longer term 1950-2016 trend of +0.100°C decade-1. Global annual 
                         mean sea level also reached a new record high, marking the sixth 
                         consecutive year of increase. Global annual ocean heat content saw 
                         a slight drop compared to the record high in 2015. Alpine glacier 
                         retreat continued around the globe, and preliminary data indicate 
                         that 2016 is the 37th consecutive year of negative annual mass 
                         balance. Across the Northern Hemisphere, snow cover for each month 
                         from February to June was among its four least extensive in the 
                         47-year satellite record. Continuing a pattern below the surface, 
                         record high temperatures at 20-m depth were measured at all 
                         permafrost observatories on the North Slope of Alaska and at the 
                         Canadian observatory on northernmost Ellesmere Island. In the 
                         Antarctic, record low monthly surface pressures were broken at 
                         many stations, with the southern annular mode setting record high 
                         index values in March and June. Monthly high surface pressure 
                         records for August and November were set at several stations. 
                         During this period, record low daily and monthly sea ice extents 
                         were observed, with the November mean sea ice extent more than 5 
                         standard deviations below the 1981-2010 average. These record low 
                         sea ice values contrast sharply with the record high values 
                         observed during 2012-14. Over the region, springtime Antarctic 
                         stratospheric ozone depletion was less severe relative to the 
                         1991-2006 average, but ozone levels were still low compared to 
                         pre-1990 levels. Closer to the equator, 93 named tropical storms 
                         were observed during 2016, above the 1981-2010 average of 82, but 
                         fewer than the 101 storms recorded in 2015. Three basins-the North 
                         Atlantic, and eastern and western North Pacific-experienced 
                         above-normal activity in 2016. The Australian basin recorded its 
                         least active season since the beginning of the satellite era in 
                         1970. Overall, four tropical cyclones reached the Saffir-Simpson 
                         category 5 intensity level. The strong El Niño at the beginning of 
                         the year that transitioned to a weak La Niña contributed to 
                         enhanced precipitation variability around the world. Wet 
                         conditions were observed throughout the year across southern South 
                         America, causing repeated heavy flooding in Argentina, Paraguay, 
                         and Uruguay. Wetter-than-usual conditions were also observed for 
                         eastern Europe and central Asia, alleviating the drought 
                         conditions of 2014 and 2015 in southern Russia. In the United 
                         States, California had its first wetter-than-average year since 
                         2012, after being plagued by drought for several years. Even so, 
                         the area covered by drought in 2016 at the global scale was among 
                         the largest in the post-1950 record. For each month, at least 12% 
                         of land surfaces experienced severe drought conditions or worse, 
                         the longest such stretch in the record. In northeastern Brazil, 
                         drought conditions were observed for the fifth consecutive year, 
                         making this the longest drought on record in the region. Dry 
                         conditions were also observed in western Bolivia and Peru; it was 
                         Bolivia's worst drought in the past 25 years. In May, with 
                         abnormally warm and dry conditions already prevailing over western 
                         Canada for about a year, the human-induced Fort McMurray wildfire 
                         burned nearly 590000 hectares and became the costliest disaster in 
                         Canadian history, with \$3 billion (U.S. dollars) in insured 
                         losses.",
                  doi = "10.1175/2017BAMSStateoftheClimate.2",
                  url = "http://dx.doi.org/10.1175/2017BAMSStateoftheClimate.2",
                 issn = "0003-0007",
                label = "isi 2017-120-05 
                         
                         Aaron-MorrisonAAAAAAAAAAAAAAABBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBCCCCCCCCCCCCCCCCCCCCCCCCDEJLDDDDDDDDDDDDDDDDDDDDDDDDEEEEEFFFFFFFFFFFFFFFFFFFFFFFGGGGGGGGGGGGGGHHHHHHHHHHHHHHHHHHHHHHHHHHIIIIIIJJJJJJJJJJJKKKKKKKKKKKKKKKKKKKKKKKKKKKLLLLLLLLLLLLLLLLLLLLLLLLLLMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMMNNNNNNOOOOPPPPPPPPPPPPPPPPPPPPPPPQQRRRRRRRRRRRRRRRRRRRRRRSSSSSSSSSSSSSSSSSSSSSSSSSSSSSSSSSSSSSSSSTTTTTTTTTTTTTTTTTTVVAVVVVVVVVVVWWWWWWWWWWWWWWWWWWWWWWWWWWXYYYYYZZZZZZLGMOSVAGMRY:2017:StCl20",
             language = "en",
           targetfile = "state.pdf",
                  url = "https://www.scopus.com/inward/record.uri?eid=2-s2.0-85028835793\&doi=10.1175%2f2017BAMSStateoftheClimate.2\&partnerID=40\&md5=b977ef5ed8631069d7e52fb8fc5c82c1",
        urlaccessdate = "27 abr. 2024"
}


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