Little ice age glacier history of the central and western alps from pictorial documents

The Lower Grindelwald Glacier (Bernese Oberland, Switzerland) consists of two parts, the Ischmeer in the east (disconnected) and the Bernese Fiescher Glacier in the west. During the Little Ice Age (LIA), the glacier terminated either in the area of the “Schopffelsen” (landmark rock terraces) or advanced at least six times (ten times if we include early findings) even further down into the valley bottom forming the “Schweif” (tail). Maximal ice extensions were reached in 1602 and 1855/56 AD. The years after the end of the LIA have been dominated by a dramatic melting of ice, especially after 2000. The Mer de Glace (Mont Blanc area, France) is a compound valley glacier formed by the tributaries Glacier du Tacul, Glacier de Léschaux, and Glacier de Talèfre (disconnected). During the LIA, the Mer de Glace nearly continuously reached the plain in the Chamonix Valley (maximal extensions in 1644 and 1821 AD). The retreat, beginning in the mid-1850s, was followed by a relatively stable position of the front (1880s until 1930s). Afterwards the retreat has continued until today, especially impressive after 1995. The perception of glaciers in the early times was dominated by fear. In the age of Enlightenment and later in the 19th century, it changed to fascination. In the 20th century, glaciers became a top attraction of the Alps, but today they are disappearing from sight. With a huge number of high-quality pictorial documents, it is possible to reconstruct the LIA history of many glaciers in the European Alps from the 17th to the 19th centuries. Thanks to these pictures, we get an image of the beauty and fascination of LIA glaciers, ending down in the valleys. The pictorial documents (drawings, paintings, prints, photographs, and maps) of important artists (Caspar Wolf, Jean-Antoine Linck, Samuel Birmann) promoted a rapidly growing tourism. Compared with today’s situations, it gives totally different landscapes – a comparison of LIA images with the same views of today is probably the best visual proof for the changes in climate

The Glacier Views of Jean-Antoine Linck – A Milestone for the Mont Blanc Glacier History from the 18th to the 19

Interdisciplinary approaches are needed to reconstruct the behaviour of glaciers beyond the beginning of systematic measurements. For example, historical documents have been used to reconstruct former glacier extents successfully at different sites, including in the well-documented Mont Blanc area that became popular since the mid-18th century among artists, scientists, and travellers. Jean-Antoine Linck from Geneva is probably the artist to whom we owe the greatest number of unique glacier views. Linck’s special preference were the ice regions, which he discovered and drew with alpinistic daring and naturalistic correctness, preferably by gouache, although many pencil sketches are preserved. Linck subtly used the etching technique to create easily reproducible plates in large format, which are then hand-coloured with gouache and watercolour. This technique allowed him to create numerous reproductions of the same view, while still giving them a unique and original aspect, views that are remarkable for their serenity and silence, while offering luminous atmospheres. These illustrations introduced the realistic representation of the high mountains into the iconography of Genevese painting and thus led to a new kind of landscape painting with a permanent character. From a perspective of glacier history and although many of his artworks are not exactly dated by the author, the work of Jean-Antoine Linck is indispensable since it represents the whole development, specifically of the Mer de Glace and the Glacier des Bossons, but also other glaciers during the period from the end of the 18th century until the 19th century glacier maximum around 1820. Linck’s work has the same importance for the Mont Blanc area as that of Caspar Wolf and Samuel Birmann for the central Swiss Alps or Thomas Ender for the Austrian Alps in terms of glacier iconography. Therefore, Linck was both an artist and a glacier historian. // Des approches interdisciplinaires sont nécessaires pour reconstruire les fluctuations des glaciers au xixe siècle, au-delà du début des mesures systématiques. Par exemple, des documents historiques ont été appliqués pour reconstituer d’anciennes étendues des glaciers sur différents sites, notamment dans la région du Mont-Blanc, qui sont très bien documentés et devenus populaires parmi les artistes, les scientifiques et les voyageurs depuis le milieu du xviiie siècle. Le Genevois Jean-Antoine Linck est probablement l’artiste à qui l’on doit le plus de vues glaciaires exceptionnelles. La préférence particulière de Linck était les régions des glaciers, qu’il a découvertes et dessinées avec une audace d’alpiniste et une exactitude de naturaliste, principalement à la gouache, bien que de nombreux croquis au crayon aient été conservés. Linck a subtilement utilisé la technique de la gravure pour créer des planches de grand format facilement reproductibles, qui ont été ensuite coloriées à la gouache et à l’aquarelle. Cette technique lui a permis de créer de nombreuses reproductions d’une même vue, tout en leur donnant un aspect unique et original. Elles sont remarquables de sérénité et de silence, tout en offrant des ambiances lumineuses. Ces illustrations introduisent la représentation réaliste de la haute montagne dans l’iconographie de la peinture genevoise et conduisent ainsi à une nouvelle forme de peinture de paysage à caractère permanent. D’un point de vue de l’histoire des glaciers, et bien que nombre de ses œuvres ne soient pas exactement datées par l’auteur, l’ouvrage de Jean-Antoine Linck est indispensable. Il représente l’ensemble de l’évolution de la mer de Glace et du glacier des Bossons, mais également d’autres glaciers, pendant la période allant de la fin du xviiie siècle jusqu’au maximum glaciaire du xixe siècle vers 1820. L’œuvre de Linck accorde au territoire du Mont-Blanc la même importance, en termes d’iconographie des glaciers, que celle de Caspar Wolf et Samuel Birmann pour les Alpes centrales suisses, ou de Thomas Ender pour les Alpes autrichiennes. Linck était donc à la fois artiste et historien des glaciers

Last phase of the Little Ice Age forced by volcanic eruptions

During the first half of the nineteenth century, several large tropical volcanic eruptions occurred within less than three decades. The global climate effects of the 1815 Tambora eruption have been investigated, but those of an eruption in 1808 or 1809 whose source is unknown and the eruptions in the 1820s and 1830s have received less attention. Here we analyse the effect of the sequence of eruptions in observations, global three-dimensional climate field reconstructions and coupled climate model simulations. All the eruptions were followed by substantial drops of summer temperature over the Northern Hemisphere land areas. In addition to the direct radiative effect, which lasts 2–3 years, the simulated ocean–atmosphere heat exchange sustained cooling for several years after these eruptions, which affected the slow components of the climate system. Africa was hit by two decades of drought, global monsoons weakened and the tracks of low-pressure systems over the North Atlantic moved south. The low temperatures and increased precipitation in Europe triggered the last phase of the advance of Alpine glaciers. Only after the 1850s did the transition into the period of anthropogenic warming start. We conclude that the end of the Little Ice Age was marked by the recovery from a sequence of volcanic eruptions, which makes it difficult to define a single pre-industrial baseline

The Little Ice Age history of the Glacier des Bossons (Mont Blanc massif, France): a new high-resolution glacier length curve based on historical documents

Historical and proxy records document that there is a substantial asynchronous development in temperature, precipitation and glacier variations between European regions during the last few centuries. The causes of these temporal anomalies are yet poorly understood. Hence, highly resolved glacier reconstructions based on historical evidence can give valuable insights into past climate, but they exist only for few glaciers worldwide. Here, we present a new reconstruction of length changes for the Glacier des Bossons (Mont Blanc massif, France), based on unevaluated historical material. More than 250 pictorial documents (drawings, paintings, prints, photographs, maps) as well as written accounts have been critically analysed, leading to a revised picture of the glacier’s history, especially from the mid-eighteenth century up to the 1860s. Very important are the drawings by Jean-Antoine Linck, Samuel Birmann and Eugène Viollet-le Duc, which depict meticulously the glacier’s extent during the vast advance and subsequent retreat during the nineteenth century. The new glacier reconstruction extends back to AD 1580 and proves maxima of the Glacier des Bossons around 1610/1643, 1685, 1712, 1777, 1818, 1854, 1892, 1921, 1941, and 1983. The Little Ice Age maximum extent was reached in 1818. Until the present, the glacier has lost about 1.5 km in length, and it is now shorter than at any time during the reconstruction period. The Glacier des Bossons reacts faster than the nearby Mer de Glace (glacier reconstruction back to AD 1570 available). The Mont Blanc area is, together with the valley of Grindelwald in the Swiss Alps (two historical glacier reconstructions available back to AD 1535, and 1590, respectively), among the two regions that are probably best-documented in the world regarding historical glacier data