108 Graphs From 89 New Papers Invalidate Claims Of Unprecedented Global-Scale Modern Warmth

By: - Climate DepotAugust 3, 2018 3:09 PM

108 Graphs From 89 New Papers Invalidate Claims Of Unprecedented Global-Scale Modern Warmth


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108 Graphs From 89 New Papers Invalidate Claims Of Unprecedented Global-Scale Modern Warmth

by Kenneth Richard / Yesterday, 05:15

During 2017, there were 150 graphs from 122 scientific papers published in peer-reviewed journals indicating modern temperatures are not unprecedented, unusual, or hockey-stick-shaped — nor do they fall outside the range of natural variability. We are a little over halfway through 2018 and already 108 graphs from 89 scientific papers undermine claims that modern era warming is climatically unusual.

For the sake of brevity, just 13 (15%) of the 89 new papers are displayed below.

The rest of the non-hockey-stick scientific papers and graphs published thus far in 2018 can be viewed by clicking the link below.

Non-Global Warming Graphs (2018 & 2017)

The list is also readily available on the NoTricksZone sidebar menu for easy reference.

Wang et al., 2018

The average RAN15-MAAT of 18.4°C over the most recent part of the record (<0.8 ka BP) [the last 800 years BP] overlaps with the range of MAATs, ca. 16.2°C to 18.7°C (av. 17.5°C) measured since 1952 at the nearest meteorological station (Yichang, located ca. 100 km away) and is very close to the av. MAAT of 18°C measured directly outside the cave by a temperature logger between 2004 and 2007 (Hu et al., 2008a). This agreement between reconstructed temperatures and instrumental measurements increases our confidence in the potential of the RAN15 proxy. RAN15-MAATs in HS4 vary from 16.5°C to 20.6°C (av. 19°C), during the last 9 ka BP, and broadly follow a long-term trend of declining temperatures in line with declining solar insolation at 30°N in July (Laskar et al., 2004). … Interestingly, the most recent 0.9 ka BP [900 years BP] is distinguished by greater variability with the highest (20.5°C) and lowest (16.5°C) RAN15-MAATs occurring consecutively at 0.6 ka BP [600 years BP] and 0.5 ka BP [500 years BP].” [Surface temperatures dropped by -4.0°C within ~100 years.]

Badino et al., 2018

Between ca. 8.4-4 ka cal BP [8,400 to 4,000 years before present], our site [Italian Alps] experienced a mean TJuly of ca. 12.4 °C, i.e. 3.1 °C warmer than today [9.3 °C]. … Between 7400 and 3600 yrs cal BP, an higher-than-today forest line position persisted under favorable growing conditions (i.e. TJuly at ca. 12 °C).”

Haddam et al., 2018

“The MD07-3100 SSST [summer sea surface temperature] reconstruction displays values ranging from 8° to 17°C over the last 21 kyr. Lowest temperatures are recorded at 18 kyr just before the onset of the deglaciation, while the warmest ones are recorded at 15 kyr (15-17°C), from 11 to 10 kyr and from 4.7 to 3 kyr. After 6.5 kyr, SSSTs stay mostly 15°C and are marked by two short-term warming events up to ~18°C, at 4.7 and 3.1 kyr respectively until reaching the present-day summer temperature values at the core location. … Core MD07-3088 displays SSST values ranging from 7 to 18°C over the last 21.4 kyr. The lowest values are observed from 18.3 to 16.5 kyr, while the highest are recorded during the middle to late Holocene (at 5.7, 1.5 and 0.7 kyr respectively). The Early Holocene, from 11.5 kyr to 10 kyr, is characterized by SSST values at around 13°C followed by a progressive 1.5°C decreasing trend until 7.7 kyr. Then a sharp SSST increase culminated at 5.8 kyr (~16°C) before decreasing again at 4.5 kyr. … The UK 37 SST reconstructions for core MD07-3088 show similar trends compared to MAT-SSST displaying the lowest and highly variable temperatures between 21 and 18 kyr. [A] sharp SST increase (~5°C) marks the Early Holocene (~10.4 kyr). Between 10.4 and 6.5 kyr, SST decreased again, followed by a plateau until 3 kyr with mean values of 13°C. Finally, after an abrupt SST rise (~2°C) centered at 1.5 kyr, UK 37 SST decrease until present-day. … The MAT SSST reconstruction of core MD07-3082 shows values ranging from 9°C to 13°C over the last 22 kyr. The lowest temperatures are recorded between 22 and 20.5 kyr, whereas a progressive SSST increase representing the last deglaciation culminates at 14.3 kyr. A two-step SSST lowering of about 3°C is recorded between 14.3 and 12.9 kyr and attributed to the ACR before reaching stable values at 12°C during the Holocene.”

Wu et al., 2018

“Summer temperatures (MJT) at Xingyun Lake in the late glacial were low, increased during the early Holocene, were highest during the middle Holocene, and then decreased during the late Holocene. The range of inferred values [for the Holocene] was 21.0°- 26.5°C. The pollen inferred temperature derived from surface samples (21.2°C), is close to the modern instrumental July temperature in Kunming (22°C), supporting the reliability of reconstructions from down-core pollen assemblages.” [Modern temperatures are 1.0°C above the coldest of the last 14,000 years, and 4.5°C cooler than the warmest temperatures of the last 14,000 years.]

Zheng et al., 2018

“In this study we present a detailed GDGT data set covering the last 13,000 years from a peat sequence in the Changbai Mountain in NE China. The brGDGT-based temperature reconstruction from Gushantun peat indicates that mean annual air temperatures in NE China during the early Holocene were 5–7°C higher than today. Furthermore, MAAT records from the Chinese Loess Plateau also suggested temperature maxima 7–9°C higher than modern during the early Holocene (Peterse et al., 2014; Gao et al., 2012; Jia et al., 2013). Consequently, we consider the temperatures obtained using the global peat calibration to be representative of climate in (NE) China. … The highest temperatures occurred between ca. 8 and 6.8 kyr BP, with occasional annual mean temperatures >8.0 ± 4.7°C, compared to the modern-day MAAT of ∼3°C.”

Ramos-Román et al., 2018

Stelling et al., 2018

Løvstrand Svarva 2018 et al., 2018

“A ring-width Pinus sylvestris chronology from Sogndal in western Norway was created, covering the period AD 1240–2008 and allowing for reconstruction of monthly mean July temperatures. This reconstruction is the first of its kind from western Norway and it aims to densify the existing network of temperature-sensitive tree-ring proxy series to better understand past temperature variability in the ‘Little Ice Age’ and diminish the spatial uncertainty. Spatial correlation reveals strong agreement with temperatures in southern Norway, especially on the western side of the Scandinavian Mountains. Five prominent cold periods are identified on a decadal timescale, centred on 1480, 1580, 1635, 1709 and 1784 and ‘Little Ice Age’ cooling spanning from 1450 to the early 18th century. High interannual and decadal agreement is found with an independent temperature reconstruction from western Norway, which is based on data from grain harvests and terminal moraines.”

Grieman et al., 2018

Lansner and Pepke Pedersen, 2018

“In locations best sheltered and protected against ocean air influence, the vast majority of thermometers worldwide trends show temperatures in recent decades rather similar to the 1920–1950 period. This indicates that the present-day atmosphere and heat balance over the Earth cannot warm areas – typically valleys – worldwide in good shelter from ocean trends notably more than the atmosphere could in the 1920–1950 period. … [T]he lack of warming in the OAS temperature trends after 1950 should be considered when evaluating the climatic effects of changes in the Earth’s atmospheric trace amounts of greenhouse gasses as well as variations in solar conditions.”

Kullman, 2018 (Scandes, Northern Sweden)

“The present paper reports results from an extensive project aiming at improved understanding of postglacial subalpine/alpine vegetation, treeline, glacier and climate history in the Scandes of northern Sweden. The main methodology is analyses of mega fossil tree remnants, i.e. trunks, roots and cones, recently exposed at the fringe of receding glaciers and snow/ice patches. This approach has a spatial resolution and accuracy, which exceeds any other option for tree cover reconstruction in high-altitude mountain landscapes. … All recovered tree specimens originate from exceptionally high elevations, about 600-700 m atop of modern treeline positions. … Conservatively drawing on the latter figure and a summer temperature lapse rate of 0.6 °C per 100 m elevation (Laaksonen 1976), could a priori mean that, summer temperatures were at least 4.2 °C warmer than present around 9500 year before present. However, glacio-isostatic land uplift by at least 100 m since that time (Möller 1987; Påsse & Anderson 2005) implies that this figure has to be reduced to 3.6 °C higher than present-day levels, i.e. first decades of the 21st century. Evidently, this was the warmth peak of the Holocene, hitherto. This inference concurs with paleoclimatic reconstructions from Europe and Greenland (Korhola et al. 2002; Bigler et al. 2003; Paus 2013; Luoto et al. 2014; Väliranta et al. 2015).”

McFarlin et al., 2018 (Greenland/Baffin Bay)

“(Greenland) Early Holocene peak warmth has been quantified at only a few sites, and terrestrial sedimentary records of prior interglacials are exceptionally rare due to glacial erosion during the last glacial period. Here, we discuss findings from a lacustrine archive that records both the Holocene and the Last Interglacial (LIG) from Greenland, allowing for direct comparison between two interglacials. Sedimentary chironomid assemblages indicate peak July temperatures [Greenland]4.0 to 7.0 °C warmer than modern during the Early Holocene maximum [10,000 to 8,000 years ago] in summer insolation. Chaoborus and chironomids in LIG sediments indicate July temperatures at least 5.5 to 8.5 °C warmer than modern.”

Bartels et al., 2018 (North Atlantic Region)

“During summer, AW [Atlantic Water] rises up to waterdepths as shallow as ~55 m. … Summer surface temperatures [1955-2012] range between up to 3°C at the northern mouth and <-1.5 °C at the southern mouth of the Hinlopen Strait, while winter surface temperatures vary between 0.5 and <~1.5°C (averaged, 1955–2012; Locarnini et al. 2013). … Increased summer insolation probably amplified the surface melting of the glaciers resulting in enhanced meltwater production and in a very high accumulation of finegrained sediments within the fjord […]. In addition, during the mild early Holocene conditions, summer sea-surface temperatures probably reaching 8–10°C [5 – 9.5°C warmer than 1955-2012] (indicated by M. edulis findings as discussed in Hansen et al. 2011) may have contributed to reducing the number of glaciers that entered the fjord directly as tidewater glaciers and thus causing a diminished IRD input. … In lake sediments from northwestern Spitsbergen a temperature drop of ~6°C is recorded between c. 7.8 and c. 7 ka [-0.8°C per century], which has been connected to a stronger influence of Arctic Water and expanding sea ice (van der Bilt et al. 2018).”