| Literature DB >> 26597713 |
Stephan Lewandowsky1, James S Risbey2, Naomi Oreskes3.
Abstract
Recent public debate and the scientific literature have frequently cited a "pause" or "hiatus" in global warming. Yet, multiple sources of evidence show that climate change continues unabated, raising questions about the status of the "hiatus". To examine whether the notion of a "hiatus" is justified by the available data, we first document that there are multiple definitions of the "hiatus" in the literature, with its presumed onset spanning a decade. For each of these definitions we compare the associated temperature trend against trends of equivalent length in the entire record of modern global warming. The analysis shows that the "hiatus" trends are encompassed within the overall distribution of observed trends. We next assess the magnitude and significance of all possible trends up to 25 years duration looking backwards from each year over the past 30 years. At every year during the past 30 years, the immediately preceding warming trend was always significant when 17 years (or more) were included in the calculation, alleged "hiatus" periods notwithstanding. If current definitions of the "pause" used in the literature are applied to the historical record, then the climate system "paused" for more than 1/3 of the period during which temperatures rose 0.6 K.Entities:
Year: 2015 PMID: 26597713 PMCID: PMC4657026 DOI: 10.1038/srep16784
Source DB: PubMed Journal: Sci Rep ISSN: 2045-2322 Impact factor: 4.379
Summary of literature on the “hiatus”.
| Article | From | To | Trend | “Slow” | “Pause” | “Hiatus” | Focus | Data |
|---|---|---|---|---|---|---|---|---|
| Allan | 2000 | 2012 | 4 | — | — | OM | H, C5, o | |
| “…energy is continuing to accumulate in the oceans, despite the apparent recent slower rates of global surface warming compared with the late twentieth century and with climate model simulations.” | ||||||||
| Brown | ≃2001 | 2012 | 3 | — | “1” | M | C5 | |
| “A slowdown in the rate of warming in the early 21st century has increased interest in unforced decadal variability within the scientific community.” | ||||||||
| Chen | ≃2001 | ≃2010 | 17 | — | 15 | O | o | |
| “The latter part of the 20th century saw rapid global warming as more heat stayed near the surface. In the 21st century, surface warming slowed as more heat moved into deeper oceans.” | ||||||||
| Clement | 2000 | 2013 | 1 | 5 | “2”+8 | O | o | |
| “A pause in global warming since 2000—a global warming ‘hiatus’—has opened up new questions about natural and human activity-driven (anthropogenic) effects on global mean trends in surface temperature.” | ||||||||
| Crowley | 1997 (2002) | 2013 | * | — | — | — | O | H, o |
| “Stable global temperatures of the last 10–15 years have been a topic of considerable discussion.” | ||||||||
| Drijfhout | ≃2001 | ≃2010 | 2 | — | 11 | O | G, H, o | |
| “…a slowing of the warming in the 2000s, even though atmospheric greenhouse gas concentrations continued to increase. This hiatus in warming may have been exaggerated by sampling errors [Cowtan and Way, 2014], but a significant slowdown is evident.” | ||||||||
| Easterling | 1998 | 2008 | — | — | — | O | N, C3 | |
| “Numerous websites, blogs and articles in the media have claimed that the climate is no longer warming, and is now cooling. Here we show that periods of no trend or even cooling of the globally averaged surface air temperature are found in the last 34 years of the observed record, and in climate model simulations of the 20th and 21st century forced with increasing greenhouse gases.” | ||||||||
| England | 2001 | 2013 | 2 | — | 27 | O | G, C5 | |
| “Despite ongoing increases in atmospheric greenhouse gases, the Earth’s global average surface air temperature has remained more or less steady since 2001.” | ||||||||
| Estrada | late 1990s | 2012 | 15 | 1 | — | O | G, H, o | |
| “The warming of the climate system is unequivocal as evidenced by an increase in global temperatures by 0.8C over the past century. However, the attribution of the observed warming to human activities remains less clear, particularly because of the apparent slow-down in warming since the late 1990s.” | ||||||||
| Fyfe | 1993 (1998) | 2012 | * >I | 2 | — | “1” | M | H, C5 |
| “Recent observed global warming is significantly less than that simulated by climate models.” | ||||||||
| Fyfe | 1993 | 2012 | * >I | — | — | 1 | M | H, C5 |
| Goddard | ≃2003 | ≃2013 | 2 | — | “1” + 7 | O | o | |
| “The ‘global warming hiatus’—the fact that globally averaged air temperatures have not increased as quickly in the past decade as they have in previous decades—is a hot topic, so to speak.” | ||||||||
| Guemas | 2000 | 2010 | 26 | 7 | 3 | O | o | |
| “Despite a sustained production of anthropogenic greenhouse gases, the Earth’s mean near-surface temperature paused its rise during the 2000–2010 period.” | ||||||||
| Haywood | 2002 | 2012 | 4 | — | 4 | M | H, o | |
| “The slow-down in global warming over the last decade has lead to significant debate about whether the causes are of natural or anthropogenic origin.” | ||||||||
| Hawkins | 1998 | 2012 | * >I | 12 | “2” + 12 | — | O | H, o |
| “The recent slowdown (or ‘pause’) in global surface temperature rise is a hot topic for climate scientists and the wider public.” | ||||||||
| Held | 1993 | 2012 | * >I | — | 1 | 10 | M | H, o |
| “A global climate model that factors in the observed temperature of the surface ocean in the eastern equatorial Pacific offers an explanation for the recent hiatus in global warming.” | ||||||||
| Huber | ≃1998 | 2012 | 3 | — | “2” + 2 | OM | H, CW, C, o | |
| “Global mean surface warming over the past 15 years or so has been less than in earlier decades and than simulated by most climate models.” | ||||||||
| Hunt | 1998 | 2010 | — | — | 22 | O | H, o | |
| “Controversy continues to prevail concerning the reality of anthropogenically-induced climatic warming. One of the principal issues is the cause of the hiatus in the current global warming trend.” | ||||||||
| Kamae | ≃1998 | 2012 | 5 | 2 | 9 | O | G, C5 | |
| “This global-warming hiatus is a period characterized by a pause in global SAT increase, despite a continued increase in radiative forcing….” | ||||||||
| Kaufmann | 1998 | 2008 | 7 | — | 8 | O | H, G, o | |
| “Given the widely noted increase in the warming effects of rising greenhouse gas concentrations, it has been unclear why global surface temperatures did not rise between 1998 and 2008.” | ||||||||
| Kosaka | 2001 | 2012 | 2 | — | 28 | M | H, o | |
| “Despite the continued increase in atmospheric greenhouse gas concentrations, the annual-mean global temperature has not risen in the twenty-first century, challenging the prevailing view that anthropogenic forcing causes climate warming.” | ||||||||
| Lin | “>decade” | NA | — | 1 | 8 | O | N, o | |
| “The recent global-warming hiatus is attributed to a La Niña-like decadal cooling phenomenon over the eastern tropical Pacific Ocean.” | ||||||||
| Lovejoy | 1998 | 2013 | “1” + 1 | “10” + 21 | “1” | M | G, o | |
| “More troubling, the models over-estimated the post-1998 El Ni | ||||||||
| Lu | unspecified | 2 | — | “1” + 15 | M | o | ||
| “The global warming hiatus does not necessarily mean a hiatus in anthropogenic greenhouse gas forcing and forced climate change….” | ||||||||
| Macias | 2001 | 2013 | 1 | — | “1” + 13 | O | H | |
| “Global surface temperature has been increasing since the beginning of the 20th century but with a highly variable warming rate, and the alternation of rapid warming periods with ‘hiatus’ decades is a constant throughout the series.” | ||||||||
| Maher | 2001 | 2013 | 1 | — | “1” + 104 | M | G, C | |
| “The latest generation of climate model simulations are used to investigate the occurrence of hiatus periods in global surface air temperature in the past and under two future warming scenarios.” | ||||||||
| McGregor | unspecified | NA | 1 | 2 | 3 | OM | G, o | |
| Meehl | 2000 | 2009 | — | — | 34 | M | o | |
| “There have been decades, such as 2000–2009, when the observed globally averaged surface-temperature time series shows little increase or even a slightly negative trend (a hiatus period).” | ||||||||
| Meehl | 2000 | 2009 | 1 | — | 79 | OM | o | |
| “Globally averaged surface air temperatures in some decades show rapid increases (accelerated warming decades), and in other decades there is no warming trend (hiatus decades).” | ||||||||
| Meehl | 2000 | 2009 | — | — | 13 | M | o | |
| Meehl | 2000 | 2013 | 2 | — | 32 | M | H, C5 | |
| “The slowdown in the rate of global warming in the early 2000s is not evident in the multi-model ensemble average of traditional climate change projection simulations.” | ||||||||
| Palmer | unspecified | NA | — | 9 | — | M | C5 | |
| Ridley | “post 2000” | 2 | “1” | “1” + 2 | O | o | ||
| “Understanding the cooling effect of recent volcanoes is of particular interest in the context of the post-2000 slowing of the rate of global warming.” | ||||||||
| Risbey | 1998 | 2012 | — | — | “1” | M | H, G, C5, CW | |
| “The differences between climate model forecasts and projections have come to prominence over interpretation of model simulations of recent temperature trends.” | ||||||||
| Santer | 1998 | 2012 | 4 | — | “3” | O | C5, o | |
| “Despite continued growth in atmospheric levels of greenhouse gases, global mean surface and tropospheric temperatures have shown slower warming since 1998 than previously.” | ||||||||
| Schmidt | 1997 | 2013 | * | 2 | — | — | M | G, CW, C5 |
| “Climate models projected stronger warming over the past 15 years than has been seen in observations.” | ||||||||
| Seneviratne | 1997 | 2012 | 4 | “1” + 5 | 5 | O | H, o | |
| “Observational data show a continued increase of hot extremes over land during the so-called global warming hiatus. This tendency is greater for the most extreme events and thus more relevant for impacts than changes in global mean temperature.” | ||||||||
| Sillmann | 1996 | 2010 | * >I | 1 | — | “1” + 10 | M | C5, o |
| “The discrepancy between recent observed and simulated trends in global mean surface temperature has provoked a debate about possible causes and implications for future climate change projections.” | ||||||||
| Smith | ≃1998 | 2012 | 11 | — | — | OM | H, G, N, C5 | |
| “…it is now clear that the rate of warming has slowed substantially over the past 15 years or so and the observations are very much at the lower end of model simulations.” | ||||||||
| Solomon | 2000 | 2009 | 1 | — | — | OM | H, G, N, o | |
| Trenberth | 2000 | 2012 | 4 | 1 | 13 | O | H, G, N, o | |
| “Global warming first became evident beyond the bounds of natural variability in the 1970s, but increases in global mean surface temperatures have stalled in the 2000s.” | ||||||||
| Trenberth | 1999 (2000) | 2012 | * | 2 | 6 | 11 | O | G, N, o |
| “Although the 2000s are by far the warmest decade on record, the rate of increase of global mean temperature since 2000 has slowed....” | ||||||||
| Watanabe | 2000 | 2009 | 4 | — | 27 | OM | H, G, C3, C5 | |
| “The rate of increase of global-mean surface air temperature… has apparently slowed during the last decade.” | ||||||||
| Watanabe | 2000 | 2009 | 3 | 2 | 14 | M | H, C3, C5 | |
| “Reasons for the apparent pause in the rise of global-mean surface air temperature… after the turn of the century has been a mystery, undermining confidence in climate projections.” | ||||||||
Figure 1Global mean surface temperature (GMST) anomalies estimated by NASA’s Goddard Institute for Space Studies (GISS) data set (40 http://data.giss.nasa.gov/gistemp/, all analyses based on dataset downloaded on 17 January 2015).
The histogram at the bottom represents the distribution of presumed start years for the presumed “hiatus” in the corpus of articles (; see Table 1) considered for this analysis. The vertical lines represent the 5th (1993) and 95th (2001) percentile, respectively, of presumed starting years for the “hiatus”. The small inset shows the overall historical temperature anomalies recorded since 1880.
Figure 2(A) distribution of observed decadal temperature trends (GISS) within the “hiatus” windows defined by the corpus of articles considered for this analysis (blue), compared to the distribution of all possible temperature trends from 1950 till 2012, the reference period used by the IPCC to establish the long-term warming trend (pink). (B) same distribution of temperature trends within the “hiatus” windows (blue) compared to the distribution of all possible temperature trends from 1964 till 2012 (pink). The year 1964 is the lower bound for the 95% confidence interval of a recent change-point analysis that sought to identify the onset of modern global warming. (C) same distribution of temperature trends within the “hiatus” windows (blue) compared to the distribution of all possible temperature trends from 1976 till 2012 (pink). The year 1976 is the upper bound for the 95% confidence interval of a recent change-point analysis that sought to identify the onset of modern global warming. In all panels, the distribution of all possible trends is obtained by computing all trends of a given duration from all possible years within the time period considered. The duration of trends is weighted by the propensity of presumed “hiatus” durations in the corpus. Thus, each 10-year trend is replicated 8 times (as 8 articles in the corpus presumed the “hiatus” to extend over 10 years), each 11-year trend 5 times, and so on. See Table 1 for details of the distribution of presumed “hiatus” durations in the corpus. The vertical red lines in each panel represents the long-term trend (1951–2012) that was used by the IPCC in their Fifth Assessment Report as a benchmark for comparison with the “hiatus.” The solid line is for the GISS dataset40 analyzed here, and the dashed line is the same long-term trend using the UK Met Office’s HadCRUT4 data set39 used by the IPCC.
Figure 3(A) Observed magnitude of temperature trends (GISS, K/decade) as a function of vantage year and the number of years included in the computation of the trend. Trends are capped at ±1 K for plotting. For each vantage year, trends are computed for all possible windows between 3 and 25 years duration, all of which end with the particular vantage year. The dots indicate which trends are significant () in an ordinary least squares analysis of annual means, and the horizontal dashed line indicates the number of years that must be included () for the trend to be significant from all vantage points. The open circles identify combinations of onset and duration that have been used to identify the “hiatus” by articles in the corpus. Multiple articles may contribute to a given circle. The Online Supplementary Material shows that the basic conclusions are unaffected by consideration of autocorrelations, although an additional 2 years are required to reach significance for all vantage points across the entire 30-year period. (B) Level of statistical significance for trends (GISS, K/decade) as a function of vantage year and the number of years included in the computation of the trend. Trends that are clearly non-significant () are shown in beige, those that approach significance () are shown in shades of gray, and significant trends () are shown in shades of terracotta. The diagonal lines identify calendar years that contribute to the analysis. Any observation in the grid that lies to the Southeast of a given line includes only observations from the stated year onward, and any observation to the Northwest also includes earlier years. The observation in the top-left corner is 1960 (i.e., looking backward 25 years from 1984).