No. The albedo decrease in these recent years is a combination of a forcing (mainly reduced cloud cover, the indirect aerosol forcing caused by a reduction of anthropogenic aerosols) and feedbacks (reduced cloud albedo and reduced surface albedo). Don't try to combine the forcings and feedbacks, especially from a limited time period, into a general statement about the entire anthropocene. We must sort out these mechanisms. We must understand both the feedbacks, which determine climate sensitivity, and the forcings. Will try to clarify in the book I'm writing, but actually it mostly can be gleaned from our Pipeline paper. Best, Jim
On Fri, Jul 5, 2024 at 12:49 AM 'Robert Tulip' via geoengineering < [email protected]> wrote: > In his January 2024 newsletter titled *Global Warming Acceleration: > Causes and Consequences*, Professor James Hansen stated that reduced > albedo since 2015 is equivalent to a sudden increase of atmospheric CO2 > from 420 to 530 ppm (bolded text in email below). > > > > I am writing to seek comment on this remarkable statement. If albedo loss > over the last decade has the same warming effect as 110 ppm CO2, this > appears to be ¾ of the effect of the historic CO2 rise from 280 to 425 ppm, > equal to 145 ppm. 110/145 = 75.8%. > > > > Does this mean darkening of the world in the last decade has had three > quarters of the warming effect of all emissions since the Industrial > Revolution? > > > > If so, that suggests an urgent impetus for solar geoengineering to slow > this accelerating feedback. > > > > Regards > > > > Robert Tulip > > *From:* James Hansen <[email protected]> > *Sent:* Saturday, January 13, 2024 3:01 AM > *Subject:* Global Warming Acceleration: Causes and Consequences > > > > View this email in your browser > <https://mailchi.mp/caa/global-warming-acceleration-causes-and-consequences?e=f99fbe43ae> > > > > A PDF of this Communication is available on my* webpage > <https://columbia.us1.list-manage.com/track/click?u=0ebaeb14fdbf5dc65289113c1&id=a1a018956b&e=f99fbe43ae>*, > along with prior Communications and other resources. > > > > [image: Tweet to your followers] > <https://columbia.us1.list-manage.com/track/click?u=0ebaeb14fdbf5dc65289113c1&id=0239cda383&e=f99fbe43ae> > > Tweet to your followers > <https://columbia.us1.list-manage.com/track/click?u=0ebaeb14fdbf5dc65289113c1&id=07537bbce5&e=f99fbe43ae> > > [image: Share on your Facebook] > <https://columbia.us1.list-manage.com/track/click?u=0ebaeb14fdbf5dc65289113c1&id=7d4fd1dfe2&e=f99fbe43ae> > > Share on your Facebook > <https://columbia.us1.list-manage.com/track/click?u=0ebaeb14fdbf5dc65289113c1&id=0dcc72dbcc&e=f99fbe43ae> > > [image: Forward to your friends] > <https://us1.forward-to-friend.com/forward?u=0ebaeb14fdbf5dc65289113c1&id=2b319f463b&e=f99fbe43ae> > > Forward to your friends > <https://us1.forward-to-friend.com/forward?u=0ebaeb14fdbf5dc65289113c1&id=2b319f463b&e=f99fbe43ae> > > > > *Fig. 1. Global temperature relative to 1880-1920 based on the GISS > analysis.[1],[2] * > > > > *Global Warming Acceleration: Causes and Consequences* > > 12 January 2024 > James Hansen, Makiko Sato, Reto Ruedy > > > > *Abstract**.* Record global temperature in 2023 helps reveal acceleration > of global warming on decadal time scales. The proximate cause of the > acceleration is increase of Earth’s energy imbalance, specifically a > substantial darkening of the planet (decreased albedo) equivalent to a CO2 > increase of more than 100 ppm, although it is difficult to apportion the > albedo change between aerosol forcing and cloud feedbacks because of > limited global measurements. Large 2023 warming is consistent with key > findings in *Global Warming in the Pipeline*:[3] reduced aerosol cooling > and high climate sensitivity. We expect record monthly temperatures to > continue into mid-2024 due to the present large planetary energy imbalance, > with the 12-month running-mean global temperature reaching +1.6-1.7°C > relative to 1880-1920 and falling to only +1.4 ± 0.1°C during the following > La Nina. Considering the large planetary energy imbalance, it will be clear > that the world is passing through the 1.5°C ceiling, and is headed much > higher, unless steps are taken to affect Earth’s energy imbalance. > > > > Global temperature in the GISS analysis increased 0.28°C in 2023, from > 1.16°C to 1.44°C (Fig. 1), the largest annual increase in the 144-year > record. This annual rise is largely due to the ongoing tropical El Nino > warming, but no prior El Nino engendered as much warming, which points to > an additional drive for global warming acceleration. We have argued[3] that > the imminent threat of human-made climate change is understated in > IPCC[4] assessments, which are based predominately on global climate models > (GCMs). We suggest that the IPCC best estimate for climate sensitivity (3°C > for 2×CO2 or 0. 75°C per W/m2) is an underestimate, as we find real-world > (paleoclimate) evidence for a sensitivity of 4.8°C ±1.2°C for 2×CO2 (1.2°C > per W/m2). In addition, we suggest that IPCC underestimates (negative) > aerosol climate forcing and global cooling by aerosols that partly > counterbalances greenhouse gas (GHG) warming. These two errors compensate > and allow GCMs with low sensitivity to match observed warming of the past > century by using an unrealistically small aerosol effect. Compensation is > not an accident; it is a result of overreliance on GCMs. With aerosol > forcing unmeasured, it is natural for modelers to focus on an aerosol > forcing that yields agreement with global warming of the past century. Some > clarification will be possible in 2024. > > Global surface temperature is well measured since about 1950,[5] but there > are large interannual fluctuations of temperature that make it difficult to > confirm a change in the rate of global warming until the change is large. > Given that the El Nino/La Nina cycle is the main cause of interannual > variability, comparison of global temperatures at the well-defined peaks of > strong El Ninos may provide potential for early detection of global warming > acceleration.[6] The three most recent strong El Ninos are 1997-98, > 2015-16, and 2023-24. The first of these was prior to reduction of > human-made aerosols. The second occurred just after the January 2015 > imposition of restrictions on sulfur content of ship fuels by the > International Maritime Organization (IMO), and the third occurred after > strengthening of the restrictions in January 2020. Fig. 2 compares global > temperatures during these years (red lines) with the prior record monthly > temperatures (gray area). > > > > > > *Fig. 2. Global temperature during El Nino origin years (left side) and El > Nino peak years, compared with monthly record high temperatures prior to > the last three strong El Ninos.* > > > > The strong 1997-98 “El Nino of the century” produced 8-9 clear global > temperature records, the 2015-2016 El Nino produced 10 clear record months, > and the 2023-24 El Nino has already produced 7 record months about half way > through the period of Nino-elevated temperature. The rate of warming > between the first two El Ninos, i.e., between 1998 and 2016, was > 0.23°C/decade, moderately larger than the 0.18°C/decade warming rate during > 1970-2010. Another eight months of temperature data are needed to assess > the warming rate between the last two El Ninos. > > > > > > *Fig. 3. Nino3.4 SST (upper panel) and temperature of ocean upper 300m in > equatorial region.[7]* > > > > Use of El Ninos as a measuring stick depends on the El Ninos being > comparable. The Nino3.4 temperature (Fig. 3) may be a flawed measure of El > Nino strength. It implies that the 2015-16 El Nino was stronger than the > “El Nino of the (20th) century” in 1997-98. A better measure is probably > the heat content anomaly in the upper 300m of the equatorial Pacific (Fig. > 3, bottom) because the 300m heat anomaly is a direct measure of the excess > heat available for expulsion to the atmosphere. The 300m heat content shows > that the three El Ninos successively decrease in magnitude, with the > 2023-24 El Nino notably unimpressive. Further discussion and illustration > of this matter is in a prior communication.[8] A declining strength of the > El Ninos only enhances our conclusions. > > *How do we know global temperature will continue to grow in the next 5-8 > months, carrying the 12-month running-mean to at least 1.6-1.7°C? The main > reason is the large increase of global absorbed solar radiation (ASR) since > 2015 (Fig. 4), which is a decrease of Earth’s albedo (reflectivity) by 0.4% > (1.4/340).[9] This reduced albedo is equivalent to a sudden increase of > atmospheric CO2 from 420 to 530 ppm.* Increase of EEI (Fig. 5) is smaller > than the increase of ASR because the warming increases thermal emission to > space. The increase of ASR since 2015 is particularly important because it > acts as a “fresh forcing,” regardless of whether it is a forcing, a > persistent feedback, or a combination thereof. Given the absence of > monitoring of global aerosol forcing, ASR provides our best clue as to the > changing drives for global warming. These assertions warrant discussion. > > > > > > *Fig. 4. Global absorbed solar radiation and Earth’s energy imbalance > relative to the mean of the first 120 months of CERES data. CERES > data[10] are available at http://ceres.larc.nasa.gov/ > <https://columbia.us1.list-manage.com/track/click?u=0ebaeb14fdbf5dc65289113c1&id=9b2861a13c&e=f99fbe43ae>* > > > > > > > *Fig. 5. Percent of equilibrium global surface temperature response to > instant CO2 doubling.[11]* > > > > Almost half of the global temperature change in response to a climate > forcing occurs within the first decade after imposition of the forcing > (Fig. 5), the remaining response requiring many decades and centuries.[10] > Earth’s energy imbalance was about 0.7 W/m2 in the first 15 years of this > century[12] and solar radiation absorbed by Earth was relatively constant > (Fig. 4). The change since 2015, especially the increase of absorbed solar > radiation, is a BFD (a big deal).[13] The magnitude, longevity, and growth > of the phenomenon rule against some unexplained natural climate > oscillation. Instead, it is likely a combination of a climate forcing(s) > and feedbacks. Our interpretation[3] is that a reduction of human-made > aerosols, especially the two-step (2015 and 2020) reduction of marine > aerosols, causes an increase of climate forcing of at least ~0.5 W/m2, > possibly as great as 1 W/m2. Aerosol modeling studies[14] report a global > climate forcing due to the change of regulations on ship emissions only of > the order of *O*(0.1 W/m2), while we suggest a forcing *O*(1 W/m2), i.e., > at least ~0.5 W/m2. Despite the absence of global monitoring of the > aerosol climate forcing, it should be possible to resolve this issue within > the next few years with the help of the great inadvertent aerosol > experiment caused by the sharp imposition by the International Maritime > Organization of rule changes on ship emissions. > > The significant climate feedbacks that affect ASR are changes of sea ice > and clouds. There is little trend of Arctic sea ice since 2015. The large > loss of Antarctic sea ice in the past year may contribute to the spike in > absorbed solar radiation in the last few months of data in Fig. 4, which > will be testable from the geographic and seasonal variation of the observed > ASR. Analysis of cloud feedbacks will be more difficult because both the > aerosol forcing and cloud feedbacks operate via cloud changes, but > superficial examination of the ASR data supports the idea of an aerosol > forcing *O*(1 W/m2) as well as a significant cloud feedback (Fig. 22 in > *Pipeline* paper). > > Our interpretation – that aerosol forcing changes constitute a substantial > fraction of the change of ASR, not ~ 0.1 W/m2 – seems to place us at odds > against another community: aerosol/climate modeling. We wonder, however, > whether the small values from aerosol models are not influenced by the > expected results based on IPCC aerosol estimations. There is still large > uncertainty in aerosol modeling. As noted above, the situation may be > clarified within the next few years, which will be none too soon, as better > understanding is required for policy considerations. > > > > > > *Fig. 6. Global temperature relative to 1880-1920 based on the GISS > analysis.[1],[2] Projected El Nino warming and La Nina cooling discusses in > text and decadal acceleration in **Pipeline**.[3]* > > > > *Summary**.* > > Empirical evidence related to aerosol climate forcing will become clearer > soon. If the forcing change is as large as we believe, it will push global > warming to at least +1.6-1.7°C (Fig. 6), well above the level that would be > expected for the moderate ongoing El Nino, and it should also limit the > decline of global temperature following the El Nino. > > The coupled aerosol forcing & climate sensitivity issue is not unrelated > to the coupled ocean overturning & sea level issue that spurred the writing > of the *Pipeline* paper. In both cases, we assert that IPCC has excessive > reliance on global models with inadequate attention to analyses that pay > comparable attention to paleoclimate information, global models, and > evidence from ongoing observed climate changes. A case in point is the > present tug-of-war occurring in the Southern Ocean. Global warming seems to > be pushing the sea ice boundary south, diminishing sea ice cover. But we > found in our *Ice Melt* paper[15] that freshwater injection from observed > shrinking of ice shelf volume was already sufficient to begin cooling of > the Southern Ocean mixed layer, pushing the sea ice area north. This topic > is discussed in one of our recent communications.[16] > > This story is to be continued. The climate situation needs to be clarified > in the next several years, as that clarification will help define the > actions that are needed to assure a bright future for young people and > future generations. We appreciate your concerns and support. We are > grateful to the people who responded to our appeal for support[15] of > Climate Science, Awareness and Solutions, thus helping assure an additional > perspective in the discussion of actions needed to address ongoing global > climate change. > > > > [1] Lenssen NJL, Schmidt GA, Hansen JE *et al.* Improvements in the > GISTEMP uncertainty model > <https://columbia.us1.list-manage.com/track/click?u=0ebaeb14fdbf5dc65289113c1&id=ebc5baab04&e=f99fbe43ae> > ,* J Geophys Res Atmos* 2019;*124(12)*:6307-26 > [2] Hansen J, Ruedy R, Sato M *et al.* Global surface temperature change > <https://columbia.us1.list-manage.com/track/click?u=0ebaeb14fdbf5dc65289113c1&id=5063fc5139&e=f99fbe43ae> > . Rev Geophys 2010;*48*:RG4004 > [3] Hansen J, Sato M, Simons L *et al*. Global warming in the pipeline > <https://columbia.us1.list-manage.com/track/click?u=0ebaeb14fdbf5dc65289113c1&id=c167fec112&e=f99fbe43ae>. > *Oxford Open Clim Chan* 2023;3(1):kgad008, doi.org/10.1093/oxfclm/kgad008 > [4] IPCC. *Climate Change 2021: The Physical Science Basis > [Masson-Delmotte V, Zhai P, Pirani A et al. (eds)]. *Cambridge and New > York: Cambridge University Press, 2021 > [5] There were still significant flaws in the World War II period because > of limited and changing sources for sea surface temperature data. See > Hansen J, Sato M, Kharecha P *et al.* Young people's burden: requirement > of negative CO2 emissions. > <https://columbia.us1.list-manage.com/track/click?u=0ebaeb14fdbf5dc65289113c1&id=9fe03810e7&e=f99fbe43ae>* > Earth Syst Dyn* 2017;*8*:577-616 > [6] Grantham, J., The Race of Our Lives Revisited > <https://columbia.us1.list-manage.com/track/click?u=0ebaeb14fdbf5dc65289113c1&id=bb89d85861&e=f99fbe43ae>, > GMO White Paper, August 2018 > [7] Nino3.4 data are ERSSTv5 (1991-2020 base period) for 5°S-5°N, > 170-120°W > <https://columbia.us1.list-manage.com/track/click?u=0ebaeb14fdbf5dc65289113c1&id=146ba2a470&e=f99fbe43ae>, > while the equatorial upper 300m temperature data use 1981-2010 base > period.for 5°S-5°N, 180-100°W > <https://columbia.us1.list-manage.com/track/click?u=0ebaeb14fdbf5dc65289113c1&id=7ac9f59ef9&e=f99fbe43ae> > 1744 > [8] Hansen, J, Sato M, Ruedy, R. Global warming acceleration: El Nino > measuring stick looks good > <https://columbia.us1.list-manage.com/track/click?u=0ebaeb14fdbf5dc65289113c1&id=6c348cff61&e=f99fbe43ae>, > 14 December 2023 > [9] The average solar energy incident on Earth is about 340 W/m2. > [10] Loeb NG, Johnson GC, Thorsen, TJ *et al.* Satellite and ocean data > reveal marked increase in Earth’s heating rate > <https://columbia.us1.list-manage.com/track/click?u=0ebaeb14fdbf5dc65289113c1&id=7ac1e00654&e=f99fbe43ae>. > *Geophys Res Lett* 2021;*48*:e2021GL09304 > [11] The graph shows results for two Goddard Institute for Space Studies > GCMs defined in the *Pipeline* paper, but the approximate 100-year > e-folding time for surface temperature response is common to most global > climate models. > [12] Miniere A, von Schuckmann K, Sallee JB, Vogt L. Robust acceleration > of Earth system heating observed over the past six decades > <https://columbia.us1.list-manage.com/track/click?u=0ebaeb14fdbf5dc65289113c1&id=09c8f92297&e=f99fbe43ae>. > *Nature Sci. Rept*;13: 22975. 2023/ > https://doi.org/10.1038/s41598-023-49353-1 > [13] Climate Emergency Forum. Nov 26, 2023. Dr. James E. Hansen in > Conversation with Paul Beckwith [Video]. YouTube: > https://www.youtube.com/watch?v=WTWUJ8Lvl-U&t=1s > <https://columbia.us1.list-manage.com/track/click?u=0ebaeb14fdbf5dc65289113c1&id=acb104ce62&e=f99fbe43ae> > [14] Diamond MS. Detection of large-scale cloud microphysical changes and > evidence for decreasing cloud brightness within a major shipping corridor > after implementation of the International Maritime Organization 2020 fuel > sulfur regulations > <https://columbia.us1.list-manage.com/track/click?u=0ebaeb14fdbf5dc65289113c1&id=f84966a10e&e=f99fbe43ae>, > *Atmos Chem Phys* 2023;*23*:8259-69 > [15] Hansen J, Sato M, Hearty P *et al.* Ice melt, sea level rise and > superstorms: evidence from paleoclimate data, climate modeling, and modern > observations that 2 C global warming could be dangerous > <https://columbia.us1.list-manage.com/track/click?u=0ebaeb14fdbf5dc65289113c1&id=2fd2b03b9a&e=f99fbe43ae> > . *Atmos Chem Phys *2016;*16*:3761-812 > [16] Hansen J, Kharecha P, Sato M. 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All rights > reserved.* > > > Want to change how you receive these emails? > > You can update > <https://columbia.us1.list-manage.com/profile?u=0ebaeb14fdbf5dc65289113c1&id=2256fd804a&e=f99fbe43ae&c=2b319f463b> > your preferences or unsubscribe > <https://columbia.us1.list-manage.com/unsubscribe?u=0ebaeb14fdbf5dc65289113c1&id=2256fd804a&e=f99fbe43ae&c=2b319f463b> > from this list. > > > > > -- > > Jim Hansen, Director > > Climate Science, Awareness and Solutions Program > > Columbia University Earth Institute > > -- > You received this message because you are subscribed to the Google Groups > "geoengineering" group. > To unsubscribe from this group and stop receiving emails from it, send an > email to [email protected]. > To view this discussion on the web visit > https://groups.google.com/d/msgid/geoengineering/03f001dace96%24a959c5a0%24fc0d50e0%24%40yahoo.com.au > <https://groups.google.com/d/msgid/geoengineering/03f001dace96%24a959c5a0%24fc0d50e0%24%40yahoo.com.au?utm_medium=email&utm_source=footer> > . > -- Jim Hansen, Director Climate Science, Awareness and Solutions Program Columbia University Earth Institute -- You received this message because you are subscribed to the Google Groups "geoengineering" group. 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