[2] Lenssen, N.J.L., G.A. Schmidt, J.E. Hansen, M.J. Menne, A. Persin, R. Ruedy, and D. Zyss, 2019: Improvements in the GISTEMP uncertainty model, J. Geophys. Res. Atmos., 124, no. 12, 6307-6326, 10.1029/2018JD029522.
[3] The current GISS
analysis employs NOAA ERSST.v5 for sea surface temperature, GHCN.v4 for
meteorological stations, and Antarctic research station data, as
described in references 1 and 2.
[4] Hansen, J., M. Sato, P.
Kharecha, K. von Schuckmann, D.J. Beerling, J. Cao, S. Marcott, V.
Masson-Delmotte, M.J. Prather, E.J. Rohling, J. Shakun, P. Smith, A.
Lacis, G. Russell, and R. Ruedy, 2017: Young people's burden: Requirement of negative CO2 emissions. Earth Syst. Dynam., 8, 577-616, doi:10.5194/esd-8-577-2017.
[5] Hansen, J. and M. Sato, July Temperature Update: Faustian Payment Comes Due, www.columbia.edu/jeh1, 13 August 2021.
[6] Hansen, J., M. Sato and P. Kharecha, November Temperature Update and the Big Climate Short, www.columbia.edu/jeh1, 23 December 2021.
[7] NOAA National Center for Environmental Prediction forecasts
are available and updated weekly. A new ensemble of climate model runs
is made each week. The blue lines in Fig. 7 are the result of model runs
in the most recent release, 10 January 2022. The quantity on the
vertical axis in Fig. 7 is the temperature anomaly in the NINO3.4
region. Anomalies colder than – 0.5°C are La Nina conditions; warmer
than +0.5°C is El Nino.
[8] Hansen, J., Foreword: uncensored science is crucial for global conservation, in Conservation Science and Advocacy for a Planet in Peril: Speaking Truth to Power, ed. D.A. DellaSala, Elsevier, 2021.
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