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- W3005178207 abstract "Abstract. El Niño–Southern Oscillation (ENSO) is the strongest mode of interannual climate variability in the current climate, influencing ecosystems, agriculture, and weather systems across the globe, but future projections of ENSO frequency and amplitude remain highly uncertain. A comparison of changes in ENSO in a range of past and future climate simulations can provide insights into the sensitivity of ENSO to changes in the mean state, including changes in the seasonality of incoming solar radiation, global average temperatures, and spatial patterns of sea surface temperatures. As a comprehensive set of coupled model simulations is now available for both palaeoclimate time slices (the Last Glacial Maximum, mid-Holocene, and last interglacial) and idealised future warming scenarios (1 % per year CO2 increase, abrupt four-time CO2 increase), this allows a detailed evaluation of ENSO changes in this wide range of climates. Such a comparison can assist in constraining uncertainty in future projections, providing insights into model agreement and the sensitivity of ENSO to a range of factors. The majority of models simulate a consistent weakening of ENSO activity in the last interglacial and mid-Holocene experiments, and there is an ensemble mean reduction of variability in the western equatorial Pacific in the Last Glacial Maximum experiments. Changes in global temperature produce a weaker precipitation response to ENSO in the cold Last Glacial Maximum experiments and an enhanced precipitation response to ENSO in the warm increased CO2 experiments. No consistent relationship between changes in ENSO amplitude and annual cycle was identified across experiments." @default.
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- W3005178207 date "2020-09-28" @default.
- W3005178207 modified "2023-10-13" @default.
- W3005178207 title "Comparison of past and future simulations of ENSO in CMIP5/PMIP3 and CMIP6/PMIP4 models" @default.
- W3005178207 cites W1229488763 @default.
- W3005178207 cites W1524265891 @default.
- W3005178207 cites W1665721417 @default.
- W3005178207 cites W1683974079 @default.
- W3005178207 cites W1770994388 @default.
- W3005178207 cites W1796961055 @default.
- W3005178207 cites W1817254341 @default.
- W3005178207 cites W1869458723 @default.
- W3005178207 cites W1904760333 @default.
- W3005178207 cites W1930393311 @default.
- W3005178207 cites W1938526285 @default.
- W3005178207 cites W1949298173 @default.
- W3005178207 cites W1953339068 @default.
- W3005178207 cites W1957506591 @default.
- W3005178207 cites W1963625366 @default.
- W3005178207 cites W1968588988 @default.
- W3005178207 cites W1972458921 @default.
- W3005178207 cites W1973233492 @default.
- W3005178207 cites W1973687167 @default.
- W3005178207 cites W1977699466 @default.
- W3005178207 cites W1978389178 @default.
- W3005178207 cites W1978756482 @default.
- W3005178207 cites W1979074586 @default.
- W3005178207 cites W1982030986 @default.
- W3005178207 cites W1987258897 @default.
- W3005178207 cites W1987683141 @default.
- W3005178207 cites W1988085649 @default.
- W3005178207 cites W1991012986 @default.
- W3005178207 cites W1991564493 @default.
- W3005178207 cites W1992590047 @default.
- W3005178207 cites W1997183890 @default.
- W3005178207 cites W1998798217 @default.
- W3005178207 cites W1999224121 @default.
- W3005178207 cites W2006165291 @default.
- W3005178207 cites W2006547330 @default.
- W3005178207 cites W2007098680 @default.
- W3005178207 cites W2007177961 @default.
- W3005178207 cites W2012592445 @default.
- W3005178207 cites W2012982424 @default.
- W3005178207 cites W2013878295 @default.
- W3005178207 cites W2014145546 @default.
- W3005178207 cites W2016766950 @default.
- W3005178207 cites W2018977279 @default.
- W3005178207 cites W2022548072 @default.
- W3005178207 cites W2023432998 @default.
- W3005178207 cites W2023875545 @default.
- W3005178207 cites W2024966118 @default.
- W3005178207 cites W2026257927 @default.
- W3005178207 cites W2031806299 @default.
- W3005178207 cites W2032658276 @default.
- W3005178207 cites W2033013208 @default.
- W3005178207 cites W2033671206 @default.
- W3005178207 cites W2034387714 @default.
- W3005178207 cites W2034518773 @default.
- W3005178207 cites W2038669354 @default.
- W3005178207 cites W2039669486 @default.
- W3005178207 cites W2040718236 @default.
- W3005178207 cites W2041213163 @default.
- W3005178207 cites W2043915127 @default.
- W3005178207 cites W2045291987 @default.
- W3005178207 cites W2047294871 @default.
- W3005178207 cites W2047502570 @default.
- W3005178207 cites W2048831528 @default.
- W3005178207 cites W2052734296 @default.
- W3005178207 cites W2053685011 @default.
- W3005178207 cites W2057650592 @default.
- W3005178207 cites W2059517603 @default.