Sources for the video
Were the glaciers ever smaller before?
Swiss stone pines once grew beneath the Pasterze, so the glaciers were smaller once before. In one minute, set in the Pasterze’s own valley, the video shows why that was so back then and why the ice is going anyway today. These are its sources, statement by statement.
What the video shows
The video opens with Gustav Jägermayer’s photo of the Pasterze from 1863, exactly aligned in Google’s 3D of today: in the window the valley jumps between the ice of 1863 and today. In front of the Pasterze, the glacier stream washes out wood and peat thousands of years old, among them trunks of Swiss stone pines. Finds have been made since 1963, and again since 1990; in September 2014 a stone pine trunk 7.9 metres long. Nobody knows exactly where the trees grew: the sources place the sites under today’s ice, up to four kilometres up the valley.
So the glaciers were smaller once before; according to the dating by Kurt Nicolussi and his co-authors, the Pasterze was probably shorter than around 2010 for almost 7,000 years, from about 10,200 to 3,500 years ago. The reason back then was mainly the Earth’s orbit, which gave the summer more sun in the northern hemisphere. About 10,000 years ago, about 9 % more sunlight reached the top of the atmosphere above the Pasterze in mid-July than today, 495 instead of 455 watts per square metre.
Then the Earth’s orbit gave the summer less sun, and over millennia the glaciers grew, with retreats in between. Around 1850 they were larger than at any time in thousands of years; volcanic eruptions and a weak sun also drove that peak. Today the Earth’s orbit gives the summer just as little sun as around 1850, 455.0 against 455.4 watts per square metre. And the ice is going anyway: the window with the 1863 photo returns and jumps to today.
Back then it was mainly down to the Earth’s orbit; not this time. According to the IPCC, solar and volcanic activity have changed the Earth’s temperature since 1850–1900 by only −0.1 to +0.1 °C, while it rose by about 1.1 °C up to 2011–2020, and in Austria by about 2.9 °C up to 2023. That the glaciers have been shrinking since the 1990s is, according to the IPCC, very likely mainly due to humans.
At the end come Austria’s glaciers in their outline of around 1850, with their ice of 2021 to 2023 inside. Together, just under a third of the area is left, as the top of the panel says; 63 % of the Pasterze, half of the Hallstätter Gletscher. The video asks: which glacier is yours? And it thanks reinhardpaulseyer and Erich, whose questions in the comments it answers.
The pictures are real: Google’s photorealistic 3D of today, with the ice edges of the Pasterze around 1850, 1998, 2009 and 2022 from the Austrian Glacier Inventory, and the 1863 photo from the Albertina. The curve of the July sun is our own calculation from the orbital elements of Berger and Loutre 1991; the contour lines behind the final panel come from the geoland.at terrain model. Only the voice and the sound effects are AI-generated.
Sources and image credits
Data
- Groß and Patzelt 2015, PANGAEA · Austrian Glacier Inventory for the Little Ice Age maximum (GI LIA) (CC BY 3.0) · ice edge of the Pasterze around 1850 and, on the final panel, the outline of each glacier around 1850, the denominator of the percentages
- Kuhn et al. 2015, PANGAEA · Austrian glacier inventory GI 2, 1998 (CC BY 3.0) · ice edge of the Pasterze in 1998
- Fischer et al. 2015, PANGAEA · Austrian Glacier Inventory GI 3, 2006 (CC BY 3.0) · ice edge of the Pasterze in 2009 (GI 3 records the Glockner group in 2009)
- Hartig et al. 2026, PANGAEA · Austrian Glacier Inventory GI 5, 2021 to 2023 (CC BY 4.0) · ice edge of the Pasterze in 2022 and, on the final panel, the ice of each glacier in 2021 to 2023
- Berger and Loutre 1991, NOAA NCEI · Orbital Variations and Insolation Database: orbital elements of the Earth, 1991 solution (file orbit91) (gemeinfrei (Public Domain)) · the curve of the July sun: sunlight at the top of the atmosphere in mid-July at 47.1° north over 10,500 years, our own calculation from the orbital elements
- Data source: geoland.at (Austrian provinces) · Digital Terrain Model (DGM) Austria, 10 m (CC BY 4.0) · contour lines of the Glockner group behind the final panel, and the height at which the year labels sit on the ice edges in Google’s 3D
For the film we cropped, converted and redrew the data.
Google 3D
The Pasterze today: the view from the Franz-Josefs-Höhe, where the 1863 photo was taken (at the beginning and at the turning point), the flight above the Pasterzensee up the valley and back to the Margaritze, and the climb over the whole glacier: Google’s photorealistic 3D. In the film the credit stays in the picture for as long as Google’s image is visible: Heute in 3D: Google Maps · Kartendaten: CNES / Airbus, Airbus, Maxar Technologies, Landsat / Copernicus, Data SIO, NOAA, U.S. Navy, NGA, GEBCO
Picture
- Gustav Jägermayer (photographer), Johannesberg mit Pasterze von der Franz-Josefs Höhe aus OSO, 1863. Albertina, Vienna, inv. no. Foto2001/22/13. Licence: gemeinfrei (Public Domain). Change: cropped, rotated by 3.13° and adjusted in perspective to Google’s camera, inserted as a window labelled “1863” into Google’s 3D of today, exactly aligned from the same standpoint (the skyline lies 0.1° from Google’s in the median); at the beginning the window jumps back and forth between 1863 and today, at the turning point it returns and jumps to today at “Und das Eis geht trotzdem”.
AI, voice and music
Nothing in the film is painted or animated with AI: the 1863 photo is real, the views of today are Google’s 3D, and the ice edges, the curve and the final panel are drawn from the data. Voice and sound effects are AI-generated: the voice with Gemini 3.8 Flash TTS (“Charon”), the sound effects (glacier stream, high wind, cracking ice) with ElevenLabs. There is no music.
Each statement in the film and its sources
Swiss stone pines once grew beneath the Pasterze.
- Slupetzky, Krisai and Lieb 1998, Wiss. Mitteilungen Nationalpark Hohe Tauern 4, p. 225: trunk sections of two Swiss stone pines; the trees grew “an einem unbekannten, heute noch vergletscherten Standort im Talbecken der jetzigen Pasterzenzunge” (at an unknown site, still under ice today, in the basin of the present glacier snout)
- Slupetzky, Krisai and Lieb 1998, Wiss. Mitteilungen Nationalpark Hohe Tauern 4, p. 227: the trees grew an estimated 0.5 to 4 km further up the valley, at 2,100 to 2,300 m
- Nicolussi and Patzelt 2000, The Holocene 10, abstract p. 191: stone pine and larch, “washed out by the stream from under the present ice”
- Drescher-Schneider and Kellerer-Pirklbauer 2008, Abh. Geol. B.-A. 62, p. 47: the peat found in 2006 and 2007 also came from places “die derzeit noch unter Gletschereis und/oder unter Schutt verborgen sind” (still hidden under glacier ice or debris)
Nobody knows exactly where the stone pines grew: all sources place the sites under today’s ice. That is why the film says “beneath the Pasterze”, not “where there was ice until recently”; the lines on screen are the ice edges of 2009 and 2022, not find sites. The two main sources are not fully independent: they partly describe the same finds, and Slupetzky et al. refer to Nicolussi’s tree-ring data.
Now the meltwater is washing out their wood, thousands of years old.
- Slupetzky, Krisai and Lieb 1998, Wiss. Mitteilungen Nationalpark Hohe Tauern 4, p. 227: “Die Baum- und Torfreste wurden alle vom Gletscherbach herausgeschwemmt” (all the tree and peat remains were washed out by the glacier stream)
- Slupetzky, Krisai and Lieb 1998, Wiss. Mitteilungen Nationalpark Hohe Tauern 4, p. 225: ages of the finds from 9,180 ± 80 to 3,445 ± 70 radiocarbon years before present
- Nicolussi and Patzelt 2000, abstract p. 191: wood and peat from the early Holocene, 8100 to 6900 BC and later
- Drescher-Schneider and Kellerer-Pirklbauer 2008, Abh. Geol. B.-A. 62, p. 46: first subfossil wood as early as 1963, wood and peat again directly in front of the glacier snout since 1990
- Nicolussi et al., INQUA 2019, abstract P-2451: at a site that became ice-free in 2010, deposits from about 7,100 to 3,900 years ago, with displaced tree remains of the same period nearby
- wetter.at, 25 June 2015: “Nach 6.000 Jahren: Pasterze gibt Zirbe frei” (after 6,000 years the Pasterze releases a stone pine; a trunk 7.9 m long, discovered in September 2014)
Finds have been made since 1963, and again since 1990, as the ice retreats. Besides stone pines, Nicolussi and Patzelt also found larch; the film names the stone pine because every source names it.
Yes, the glaciers were smaller once before. But why?
- IPCC 2021, Working Group I report, chapter 2, p. 345: during the Holocene, glaciers were “at times smaller than at the end of the 20th century” (high confidence)
- Joerin et al. 2006, The Holocene 16, abstract p. 697: twelve periods in which Swiss glaciers were smaller than in 1985
- Nicolussi et al. 2020, EGU General Assembly abstract: the Pasterze was probably shorter than around 2010 from about 10,200 to 3,500 years ago
“Smaller” in the sources means smaller than at the end of the 20th century, than in 1985 or than around 2010. According to the IPCC, the glaciers of the northern hemisphere are in most places still larger today than in the early and middle Holocene (chapter 2, p. 345).
Back then the Earth’s orbit gave the summer more sun, and for almost 7,000 years the Pasterze was probably shorter than in 2009. On screen, the source: “Pasterze wohl kürzer als 2009: Nicolussi u. a. 2020” (Pasterze probably shorter than in 2009).
- Nicolussi et al. 2020, EGU General Assembly abstract “Always delayed?”: according to some 80 dates, the Pasterze was “probably at least from about 10.2 ka to about 3.5 ka continuously shorter compared to the extent around 2010 AD”
- IPCC 2021, Working Group I report, chapter 9, p. 1276: the small glaciers of the early and middle Holocene “could be attributed to high summer insolation (high confidence), unlike the current situation”; new chronologies confirm the “dominant role of orbital forcing” over millennia
- Nicolussi and Patzelt 2000, abstract p. 191: the Pasterze was smaller than in the 1990s from 8100 to 6900 BC, again by 6300 BC at the latest, and around 4800 and 3800 BC
- Joerin et al. 2006, abstract p. 697: the course of the glaciers “in line with a continuous decrease of summer insolation”
“Probably” and “almost” belong to it: the abstract says “probably”, and 10,200 to 3,500 years is 6,700 years. It compares with the extent around 2010; on screen lies the 2009 ice edge from the glacier inventory. No source traces the Pasterze individually back to the Earth’s orbit: the IPCC says it for the glaciers of the northern hemisphere, and the short Pasterze falls into the time of the strong July sun. “Earth’s orbit” stands, as in the IPCC’s “orbital forcing”, for the orbit and the tilt of the Earth’s axis.
Then it gave the summer less, and the ice grew.
- IPCC 2021, Working Group I report, chapter 9, p. 1276: in the northern hemisphere, “where summer insolation decreased during the Holocene”, “glaciers generally waxed”
- IPCC 2021, Working Group I report, chapter 2, p. 345: after their minimum 8,000 to 6,000 years ago “glaciers expanded thereafter”, up to their maximum extent between the mid-15th and the late 19th century
- Joerin et al. 2006, abstract p. 697: after 3,600 years ago the trend towards larger glaciers up to the Little Ice Age, “in line with a continuous decrease of summer insolation”
- Solomina et al. 2016, Quaternary Science Reviews 149, p. 83: from the 13th to the early 19th century, higher explosive volcanic activity made the glaciers grow, “perhaps aided by low solar irradiance forcing”
A trend over millennia, interrupted by retreats, for example in Roman times and the Middle Ages. Volcanic eruptions and a weak sun also drove the maximum around 1850; that is why the film does not say the Earth’s orbit caused it, and shows no arrow from the curve to the ice.
Around 1850 the glaciers were larger than at any time in thousands of years.
- Patzelt 2019, ANISA (Hallstätter Gletscher), p. 4: the Hallstätter Gletscher “ist seit mindestens 5000 Jahren nicht höher angestiegen als 1856 AD” (has not reached higher than in 1856 for at least 5,000 years)
- Patzelt 2019, ANISA (Hallstätter Gletscher), p. 13: the period of maximum extent of the Eastern Alpine glaciers “ist allgemein zwischen 1850 und 1860 abzugrenzen” (falls generally between 1850 and 1860)
- Schlüchter and Jörin 2004, Les Alpes 6/2004, p. 46: the Little Ice Age brought the greatest advance of the Alpine glaciers in the last ten millennia
- IPCC 2021, Working Group I report, chapter 2, p. 345: the maximum glacier extent between the mid-15th and the late 19th century
Deliberately “the glaciers”, not “the Pasterze”: for the Pasterze alone it is not documented; after the ice age it reached the Margaritze rock at each of ten to twelve maxima (Slupetzky et al. 1998, p. 226). The sentence holds for the glaciers as a whole, not for each one: some earlier advances, in the Alps too, were similar in size to those of the Little Ice Age (Solomina et al. 2016, pp. 82 f.).
Today the Earth’s orbit gives the summer just as little sun as around 1850.
- Our own calculation from the orbital elements of Berger and Loutre 1991 (NOAA, file orbit91): sunlight at the top of the atmosphere in mid-July at 47.1° north, around 1850 455.4 W/m², 1950 455.2, 2026 455.0; 2026 against 1850 −0.08 %
- Cross-check with Berger 1978 and with present-day orbital elements (NASA JPL, table 1, valid 1800 to 2050): also about −0.08 %; every measure of summer lies within 0.1 % of the value around 1850 in 2026
- IPCC 2021, Working Group I report, chapter 2, p. 297: orbital changes mainly alter how sunlight is distributed across seasons and latitudes; summer insolation at 65° north varied by only 3.2 W/m² over the past millennium
Our own calculation, checked against two further solutions for the Earth’s orbit; it applies at the top of the atmosphere, without clouds. The film deliberately does not say “as little as in over 10,000 years”: it would be true for mid-July but not for the solstice, and it was just as true around 1850.
And the ice is going anyway. On screen the 1863 photo jumps to today, then the ice edges of 1998 and 2022.
- Austrian glacier inventory GI 2 (Kuhn et al. 2015, PANGAEA): outline of the Pasterze in 1998
- GI 3 (Fischer et al. 2015, PANGAEA): outline of the Pasterze in 2009
- GI 5 (Hartig et al. 2026, PANGAEA): outline of the Pasterze in 2022
- Hartl et al. 2026, The Cryosphere 20: “accelerating glacier shrinkage and 31 % area loss within two decades” in Austria
- Solomina et al. 2016, p. 83: today’s retreat “breaks a long-term trend of increased glacier activity”
“Anyway” refers to the sentence before: the same July sun from the Earth’s orbit as around 1850, when the glaciers were at their largest.
Back then it was mainly down to the Earth’s orbit. Not this time.
- IPCC 2021, Working Group I report, chapter 9, p. 1276: the small glaciers of the early and middle Holocene, “unlike the current situation”; over millennia the “dominant role of orbital forcing”
- IPCC 2021, Working Group I report, Summary for Policymakers, p. 5: A.1.3, natural drivers, solar and volcanic activity, changed global surface temperature from 1850–1900 to 2010–2019 by only −0.1 to +0.1 °C
- IPCC 2021, Working Group I report, chapter 2, p. 297: the sun’s contribution since 1900 is small, less than about 0.1 W/m²; over millennia its output varies by about 1.5 W/m², roughly 0.1 % of its strength
- Schlüchter and Jörin 2004, Les Alpes 6/2004, p. 40: according to the authors, the wood and peat phases of the Alpine glaciers coincide with times of increased solar activity
“Mainly”, because some phases also fit a stronger sun. The film says “Earth’s orbit”, not “the sun”: the sun itself varied by only about 0.1 % over millennia, the July sun at 47° north by about 9 % because of the orbit. With “the sun” one would hear solar activity, and that does not explain the great minima.
That the glaciers have been shrinking since the 1990s is, according to the IPCC, very likely mainly due to humans.
- IPCC 2021, Working Group I report, Summary for Policymakers, p. 5: A.1.5, the human impact on the climate is “very likely the main driver of the global retreat of glaciers since the 1990s”; footnote 12: “main driver” means more than 50 % of the change
- IPCC 2021, Working Group I report, chapter 9, p. 1276: the same for the global, near-universal retreat since the 1990s
- Roe, Christian and Marzeion 2021, The Cryosphere 15: since the start of industrialisation the human share of glacier mass loss is “essentially 100 %”
- Marzeion et al. 2014, Science 345: about 69 ± 24 % human-caused from 1991 to 2010
The time reference belongs to the retreat, not to the cause: like the IPCC, the sentence says nothing about the time before 1990. “Very likely” is the IPCC’s calibrated level, “mainly” renders “main driver”, i.e. more than half; it refers to the global retreat. The film says “die Gletscher” (the glaciers) rather than “sie” (they), because after the previous sentence “sie” would mean the Earth’s orbit. The two studies feed into the IPCC’s assessment, so they are not fully independent of it.
On screen, the curve “Julisonne aus der Erdbahn” (July sun from the Earth’s orbit): on the left “rund 9 % mehr” (about 9 % more), at its tip a sun with the time below it, from “vor 10.500 Jahren” (10,500 years ago) to “vor 1.000 Jahren” (1,000 years ago), then “um 1850” (around 1850), dashed on to “heute” (today), with “genauso wenig” (just as little) above. Source on screen: “Julisonne: 47° Nord, Ausschnitt, Berger und Loutre 1991” (July sun: 47° north, detail, Berger and Loutre 1991).
- Our own calculation from the orbital elements of Berger and Loutre 1991 (NOAA, file orbit91): mid-July, 47.1° north, top of the atmosphere; maximum 495.4 W/m² about 10,000 years ago, around 1850 455.4, today 455.0, i.e. about 9 % more
- Berger and Loutre 1991, Quaternary Science Reviews 10, pp. 297–317: the solution for the Earth’s orbit that the IPCC cites for precise orbital calculations (chapter 2, p. 297)
- Cross-check with the older Berger 1978 solution from the same database (files bein1 to bein11): 8.6 % instead of 8.8 % against 1950; “about 9 %” holds for both
“July sun”, not “summer sun”: the 9 % applies to mid-July; over June to August it is about 6 %, over the summer’s total solar energy about 1 %. The vertical axis is cropped, which is why the source says “Ausschnitt” (detail); the time from 1850 to today is not to scale, hence the dashes. The curve only says “um 1850”, not “maximum”, otherwise one would read a maximum of the sun. The time below the sun counts back from today, rounded to 500 years.
On screen, the box: “Erwärmung weltweit seit 1850–1900: rund 1,1 °C (bis 2011–2020) · davon Sonne und Vulkane: −0,1 bis +0,1 °C” (global warming since 1850–1900: about 1.1 °C, up to 2011–2020; of which solar and volcanic activity: −0.1 to +0.1 °C), source on screen “Weltklimarat (IPCC) 2021”.
- IPCC 2021, Working Group I report, Summary for Policymakers, p. 5: A.1.2, “1.09 [0.95 to 1.20] °C higher in 2011–2020 than 1850–1900”
- IPCC 2021, Working Group I report, Summary for Policymakers, p. 5: A.1.3, natural drivers changed the temperature from 1850–1900 to 2010–2019 by −0.1 to +0.1 °C, humans by 1.07 °C (best estimate)
- GeoSphere Austria, CCCA Fact Sheet 50 (2024), p. 1: Austria has warmed by 2.9 °C from 1851–1900 to 2023 (“um 2,9 °C erwärmt”)
- APCC 2025, Second Austrian Assessment Report on Climate Change, key messages, p. 2: Austria is about 3.1 °C above the pre-industrial level of 1850–1900 (“um rund 3,1 °C über dem Niveau der vorindustriellen Zeit”)
- WMO, 19 March 2025: long-term global warming is now estimated “between 1.34 and 1.41 °C”
“Weltweit” (global) and the period are on screen so that nobody reads the 1.1 °C as the figure for the Pasterze: Austria has warmed considerably more, by 2.9 °C up to 2023 according to GeoSphere Austria. The IPCC gives the split into solar and volcanic activity only up to 2010–2019, which is why its figure stands with its period, although according to the WMO warming is now 1.34 to 1.41 °C.
On screen, the Pasterze’s ice edges with their years: first “Eisrand 2009” (ice edge 2009) and “2022”, from “und das Eis wuchs” (and the ice grew) also “um 1850” (around 1850), after the jump to today “1998” and “2022”. Source on screen: “Eisränder: Gletscherinventar Österreich” (ice edges: Austrian glacier inventory).
- Austrian Glacier Inventory GI LIA (Groß and Patzelt 2015, PANGAEA): outline of the Pasterze at the Little Ice Age maximum
- GI 2 (Kuhn et al. 2015, PANGAEA): the Pasterze in 1998
- GI 3 (Fischer et al. 2015, PANGAEA): the Glockner group in 2009
- GI 5 (Hartig et al. 2026, PANGAEA): the Pasterze in 2022
- Fischer et al. 2015, The Cryosphere 9, p. 763: the Little Ice Age maximum did not occur everywhere at the same time, in extreme cases “several decades” away from 1850
The years are those in which the inventories recorded the Pasterze. “Around 1850” is the maximum, which falls in a different year for each glacier. The lines lie on Google’s terrain; the year labels sit on their edge with heights from the geoland.at terrain model.
On the final panel, at the top “knapp ein Drittel übrig” (just under a third left), below it Austria’s glaciers in their outline of around 1850 with their ice of 2021 to 2023, and “Gepatschferner 66 %”, “Pasterze 63 %”, “Ochsentaler Gletscher 52 %”, “Obersulzbachkees 52 %” and “Hallstätter Gletscher 50 %”. Sources on screen: “Gletscherfläche Österreichs: Umriss um 1850, Eis 2021 bis 2023” (Austria’s glacier area: outline around 1850, ice 2021 to 2023) and “Daten: Österreichisches Gletscherinventar” (data: Austrian Glacier Inventory).
- GI LIA (Groß and Patzelt 2015, PANGAEA): the outlines around 1850
- GI 5 (Hartig et al. 2026, PANGAEA): the ice in 2021 to 2023
- Fischer et al. 2015, The Cryosphere 9, p. 759: Austria’s glaciers around 1850: 941.1 km²
- Fischer et al. 2015, The Cryosphere 9, p. 763: the area around 1850 is accurate to about ±10 %
- Hartl et al. 2026, The Cryosphere 20: 799 glaciers covering 285 ± 12 km² in 2021 to 2023
“Just under a third”: 285 km² in 2021 to 2023 against 941 km² around 1850 is 30.3 %, or 27.6 to 33.7 % given the accuracy of the area around 1850 (±10 %). The percentages of the five glaciers are our own evaluation of the two inventories: area 2021 to 2023 against area around 1850, each glacier within its outline of around 1850, fragments added up. In the Ötztal Alps, where the Gepatschferner lies, the file for around 1850 contains less area than published, so the value there may be slightly too high.
Literature and sources
- Heinz Slupetzky, Robert Krisai and Gerhard Karl Lieb: Hinweise auf kleinere Gletscherstände der Pasterze (Nationalpark Hohe Tauern, Kärnten) im Postglazial (evidence of smaller extents of the Pasterze in the postglacial: radiocarbon dates and pollen analyses), Wissenschaftliche Mitteilungen aus dem Nationalpark Hohe Tauern 4, 1998, pp. 225–240
- Kurt Nicolussi and Gernot Patzelt: Discovery of early Holocene wood and peat on the forefield of the Pasterze Glacier, Eastern Alps, Austria, The Holocene 10, 2000, pp. 191–199
- Kurt Nicolussi, Matthias Dusch, Ruth Drescher-Schneider, Andreas Kellerer-Pirklbauer and Fabien Maussion: Always delayed? Holocene and current evolution of Pasterze Glacier, Austria, EGU General Assembly 2020, EGU2020-9317 (CC BY 4.0)
- Kurt Nicolussi, Ruth Drescher-Schneider, Andreas Kellerer-Pirklbauer, Melaine Le Roy and Christian Schlüchter: Glacier evolution in the Alps during the early and mid-Holocene. New results from Tschierva and Pasterze glaciers, INQUA 2019, abstract P-2451
- Ruth Drescher-Schneider and Andreas Kellerer-Pirklbauer: Gletscherschwund einst und heute (glacier retreat then and now: new results on the Holocene vegetation and glacier history of the Pasterze), Abhandlungen der Geologischen Bundesanstalt 62, 2008, pp. 45–51
- Ulrich E. Joerin, Thomas F. Stocker and Christian Schlüchter: Multicentury glacier fluctuations in the Swiss Alps during the Holocene, The Holocene 16, 2006, pp. 697–704
- Christian Schlüchter and Ueli Jörin: Les Alpes sans glacier? Le bois et la tourbe, des indicateurs de climat, Les Alpes 6/2004, pp. 34–47 (French edition of “Alpen ohne Gletscher?”, Die Alpen 6/2004)
- Gernot Patzelt: Die prähistorische Gletscher- und Vegetationsentwicklung im Bereich des Hallstätter Gletschers (the prehistoric glacier and vegetation history around the Hallstätter Gletscher, Dachstein group), ANISA research reports 9, 2019
- Olga N. Solomina et al.: Glacier fluctuations during the past 2000 years, Quaternary Science Reviews 149, 2016, pp. 61–90
- IPCC 2021, Sixth Assessment Report, Working Group I: Summary for Policymakers (A.1.2, A.1.3, A.1.5)
- IPCC 2021, Working Group I report, chapter 2: Changing State of the Climate System (pp. 297 and 345)
- IPCC 2021, Working Group I report, chapter 9: Ocean, Cryosphere and Sea Level Change (p. 1276)
- Gerard H. Roe, John Erich Christian and Ben Marzeion: On the attribution of industrial-era glacier mass loss to anthropogenic climate change, The Cryosphere 15, 2021, pp. 1889–1905
- Ben Marzeion et al.: Attribution of global glacier mass loss to anthropogenic and natural causes, Science 345, 2014, pp. 919–921
- André Berger and Marie-France Loutre: Insolation values for the climate of the last 10 million years, Quaternary Science Reviews 10, 1991, pp. 297–317; the orbital elements as a dataset at NOAA (Orbital Variations and Insolation Database, file orbit91)
- NASA Jet Propulsion Laboratory: Approximate Positions of the Planets, table 1 (1800 to 2050), for the cross-check
- Andrea Fischer et al.: Tracing glacier changes in Austria from the Little Ice Age to the present using a lidar-based high-resolution glacier inventory in Austria, The Cryosphere 9, 2015, pp. 753–766
- Lea Hartl et al.: On thin glacial ice. New Austrian Glacier Inventory shows accelerating glacier shrinkage and 31 % area loss within two decades, The Cryosphere 20, 2026, pp. 5157–5180
- GeoSphere Austria (Barbara Chimani et al.): Bestimmung der aktuellen Klimaerwärmung für Österreich (determining current climate warming for Austria), CCCA Fact Sheet 50, December 2024
- Austrian Panel on Climate Change (APCC): Second Austrian Assessment Report on Climate Change (AAR2), key messages, June 2025
- WMO, 19 March 2025: WMO report documents spiralling weather and climate impacts
- wetter.at, 25 June 2015: Nach 6.000 Jahren: Pasterze gibt Zirbe frei (after 6,000 years the Pasterze releases a stone pine)