Premières neiges : le paysage d’hiver dans les enluminures by Alexis Metzger

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Climate reconstruction of the Little Ice Age maximum extent of the tropical Zongo Glacier using a distributed energy balance model by Autin, Philémon, Sicart, Jean Emmanuel, Rabatel, Antoine, Hock, Regine, Jomelli, Vincent

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The shifting of buffer crop repertoires in pre-industrial north-eastern Europe by Meiirzhan Abdrakhmanov, Michael Kempf, Ruta Karaliute, Piotr Guzowski, Rimvydas Lauzikas, Margaux L. C. Depaermentier, Radosław Poniat, Giedre Motuzaite Matuzeviciute

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Changement climatique et atrophie des masses glaciaires : quelles mutations pour les paysages islandais ? by Marie Chenet, Erwan Roussel

“…The Global Warming which occurs since the end of the Little Ice Age in Iceland leads to the retreat of the glacier fronts. …”
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APERÇU SUR LE CLIMAT DES SIÈCLES PASSÉS SUR LE TERRITOIRE DE LA ROUMANIE by ELENA TEODOREANU

“…It can detect known periods in Western Europe: the Little Climatic Optimum and Little Ice Age and at the end a very limited period of warming during the twentieth century…”
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Les variations récentes (1975-2000) de l’englacement dans le Massif de l’Aconcagua (Mendoza, Argentine) by Etienne Cossart, Julie Le Gall

“…The glaciers of the Aconcagua massif are currently shrinking, this trend of retreat began at the end of the Little Ice Age. The disappearance of glaciers may modify hydrological regimes. …”
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Trajectoires paysagères et crises morphosédimentaires de cônes torrentiels dans la vallée de la Maurienne (Savoie) depuis la fin du Petit Âge glaciaire by Thérèse Hugerot, Laurent Astrade, Christophe Gauchon

“…The use of numerous cadastral, cartographic, photographic and technical archives from between the 18th and 20th centuries has enabled the creation of a geohistorical information system capable of describing and characterising the landscape trajectories of these four cones since the Little Ice Age. The frequency of torrential activity and morphosedimentary crises, the industrialisation of the valley and its rural decline, major road, rail and hydroelectric developments, and the dynamics of urbanisation (and post-war reconstruction) are all factors to be taken into account in reconstructing these unique trajectories. …”
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A time-varying index for agricultural suitability across Europe from 1500–2000 by Alexander Lehner, Dylan Philippe

“…Our index captures not just long-term trends, such as the Little Ice Age, but also short-term climatic shocks. It will empower researchers to explore the interplay between climatic fluctuations and Europe’s agricultural landscape, analyze human responses at a local and regional scale, and foster a deeper understanding of the region’s historical dynamics.…”
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Recurring cycles of ice and vegetation on Baffin Island, Nunavut by Martha K. Raynolds, Helga Bültmann, Shawnee A. Kasanke, Gifford Miller, Jonathan H. Raberg

“…The most recent retreat of glaciers on Baffin Island, Nunavut, has been since the Little Ice Age, due to anthropogenic warming. Retreating cold-based ice often uncovers ancient vegetation. …”
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Central Asia Cold Case: Siberian Pine Fingers New Suspects in Growth Decline CA 1700 CE by David M. Meko, Dina F. Zhirnova, Liliana V. Belokopytova, Yulia A. Kholdaenko, Elena A. Babushkina, Nariman B. Mapitov, Eugene A. Vaganov

“…We conclude that stress from low summer temperatures in the Little Ice Age was likely exacerbated by tree damage associated with weather extremes, including infamous Mongolian “dzuds”, over 1695–1704. …”
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Greening of Svalbard in the twentieth century driven by sea ice loss and glaciers retreat by Gianmarco Ingrosso, Chiara Ceccarelli, Federico Giglio, Patrizia Giordano, Jens Hefter, Leonardo Langone, Stefano Miserocchi, Gesine Mollenhauer, Alessio Nogarotto, Mathia Sabino, Tommaso Tesi

“…Here, we measured plant-derived biomarkers from an Arctic fjord sediment core as proxies for reconstructing past changes in tundra vegetation during the transition from the Little Ice Age to modern warming. Our findings revealed a rapid expansion of the tundra since the beginning of the twentieth century, largely coinciding with the decline of summer sea ice extent and glacier retreat. …”
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Runoff responses to Atlantic multidecadal and Pacific decadal oscillations in China: Insights from the last millennium simulations by Yangyi Liu, Jie Chen, Lihua Xiong, Chong-Yu Xu

“…Taking Medieval Climate Anomaly (MCA) and Little Ice Age (LIA) as study periods and focusing on summer runoff in China, this study aims to investigate 1) the major time scales at which AMO/PDO affects runoff, and 2) the individual and coupled effects of AMO and PDO on runoff by using last millennium climate model simulations. …”
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Reconstruction of climatic events from the 16th century in Transylvania: interdisciplinary analysis based on historical sources by Ovidiu Răzvan Gaceu, Tudor Caciora, Ștefan Baias, Cezar Morar, Mihai Dudaș, Marius Stupariu, Maria Maxim

“…IntroductionUnderstanding past climate variability is essential for interpreting current and future climate trends, particularly during defining climate periods for the past two millennia, such as the Little Ice Age, which had significant socio-economic impacts.MethodsThe present study uses an interdisciplinary approach, analyzing written documents such as chronicles, diaries, and official records to extract data related to climate events in the 16th century in Transylvania (on the current territory of Romania). …”
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Nutrient cycling characteristics along a chronosequence of forest primary succession in the Hailuogou Glacier retreat area, eastern Tibetan Plateau by Danli Yang, Ji Luo, Shumiao Shu, Yan Hu, Hongsong Tang, Xuemei Li

“…Background The Hailuogou Glacier has been continuously retreating since the end of the Little Ice Age, resulting in a 125-year soil chronosequence and a complete primary forest succession sequence. …”
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