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# ANNEXES

Annexe 1: Détails des informations relatives aux datations des glaciers LGM alpins, ainsi que l'abaissement de la surface glaciaire présenté dans la Figure 2.6.

<table><thead><tr><td>Zone</td><td>Nom glacier</td><td>Age ka publié</td><td>Information</td><td>Méthode de datation</td><td>Reference</td></tr></thead><tbody><tr><td>Alpes sud</td><td>Bassin de Gesso</td><td>22,8 ka</td><td>Extension maximale</td><td>Radionucléides cosmogéniques</td><td>Federici et al. (2017)</td></tr><tr><td>Alpes sud</td><td>Rivoli-Avigliana</td><td>24,0 ± 1,5 ka</td><td>Extension maximale</td><td>Radionucléides cosmogéniques</td><td>Ivy-Ochs et al. (2018)</td></tr><tr><td>Alpes sud</td><td>Rivoli-Avigliana</td><td>19,6 ± 0,9 ka</td><td>Etape de récession</td><td>Radionucléides cosmogéniques</td><td>Ivy-Ochs et al. (2018)</td></tr><tr><td>Alpes sud</td><td>Rivoli-Avigliana</td><td>18,3-18,1 ka cal BP</td><td>Environnement déglacé</td><td><sup>14</sup>C</td><td>Larocque et Finsinger (2008)</td></tr><tr><td>Alpes sud</td><td>Ivrea</td><td>23,8 ± 1,7 ka</td><td>Extension maximale</td><td>Radionucléides cosmogéniques</td><td>Gianotti et al. (2015)</td></tr><tr><td>Alpes sud</td><td>Ivrea</td><td>20,1 ± 3,0 ka</td><td>Etape de récession</td><td>Radionucléides cosmogéniques</td><td>Gianotti et al. (2015)</td></tr><tr><td>Alpes sud</td><td>Ivrea</td><td>17,8-17,0 ka cal BP</td><td>Environnement déglacé</td><td><sup>14</sup>C</td><td>Gianotti et al. (2015)</td></tr><tr><td>Alpes sud</td><td>Orta</td><td>26,5-23 ka</td><td>Extension maximale</td><td>Radionucléides cosmogéniques</td><td>Braakhekke et al. (2020)</td></tr><tr><td>Alpes sud</td><td>Orta</td><td>19-18 ka</td><td>Etape de récession</td><td>Radionucléides cosmogéniques</td><td>Braakhekke et al. (2020)</td></tr><tr><td>Alpes sud</td><td>Verbano</td><td>25,0 ± 0,9 - 19,9 ± 0,7 ka</td><td>Extension maximale</td><td>Radionucléides cosmogéniques</td><td>Kamleitner et al. (2022)</td></tr><tr><td>Alpes sud</td><td>Verbano</td><td>19,7 ± 1,1 ka</td><td>Etape de récession</td><td>Radionucléides cosmogéniques</td><td>Kamleitner et al. (2022)</td></tr><tr><td>Alpes sud</td><td>Verbano</td><td>19,0 ka</td><td>Environnement déglacé</td><td>Radionucléides cosmogéniques</td><td>Kamleitner et al. (2022)</td></tr><tr><td>Alpes sud</td><td>Oglio (Bassin de Clusone)</td><td>26,4-25,3 ka cal BP</td><td>Extension maximale</td><td><sup>14</sup>C</td><td>Ravazzi et al. (2012a)</td></tr><tr><td>Alpes sud</td><td>Oglio (Bassin de Clusone)</td><td>18,5-17,9 ka cal BP</td><td>Environnement déglacé</td><td><sup>14</sup>C</td><td>Ravazzi et al. (2012a)</td></tr><tr><td>Alpes sud</td><td>Oglio (Lac Iseo)</td><td>18,4-18,0 ka cal BP</td><td>Environnement déglacé</td><td><sup>14</sup>C</td><td>Lauterbach et al. (2012)</td></tr><tr><td>Alpes sud</td><td>Garda</td><td>24,9-24,3 ka cal BP</td><td>Extension LGM 1</td><td><sup>14</sup>C</td><td>Monegato et al. (2017)</td></tr><tr><td>Alpes sud</td><td>Garda</td><td>23,9-23,1 ka cal BP</td><td>Extension LGM 2</td><td><sup>14</sup>C</td><td>Monegato et al. (2017)</td></tr><tr><td>Alpes sud</td><td>Garda</td><td>17,8-17,3 ka cal BP</td><td>Environnement déglacé</td><td><sup>14</sup>C</td><td>Ravazzi et al. (2014)</td></tr><tr><td>Alpes sud</td><td>Astico</td><td>24,2-23,8 ka cal BP</td><td>Etape de récession</td><td><sup>14</sup>C</td><td>Rossato et al. (2013)</td></tr><tr><td>Alpes sud</td><td>Piave</td><td>19,8-18,8 ka</td><td>Etape de récession</td><td>Radionucléides cosmogéniques</td><td>Carton et al. (2009)</td></tr><tr><td>Alpes sud</td><td>Tagliamento</td><td>28,1-24,5 ka cal BP</td><td>Extension LGM 1</td><td><sup>14</sup>C</td><td>Monegato et al. (2007)</td></tr><tr><td>Alpes sud</td><td>Tagliamento</td><td>23,4-21,5 ka cal BP</td><td>Extension LGM 2</td><td><sup>14</sup>C</td><td>Monegato et al. (2007)</td></tr><tr><td>Alpes sud</td><td>Tagliamento</td><td>21,0 ka cal BP</td><td>Etape de récession</td><td><sup>14</sup>C</td><td>Monegato et al. (2007)</td></tr><tr><td>Alpes sud</td><td>Tagliamento</td><td>20,9-19,9 ka cal BP</td><td>Environnement déglacé</td><td><sup>14</sup>C</td><td>Fontana et al. (2014)</td></tr><tr><td>Alpes sud</td><td>Sava Dolinka</td><td>23,2 ± 2,8 ka</td><td>Extension maximal</td><td>OSL</td><td>Bavec et Verbic (2011)</td></tr><tr><td>Alpes sud</td><td>Drau</td><td>18,5-18,1 ka cal BP</td><td>Environnement déglacé</td><td><sup>14</sup>C</td><td>Schmidt et al. (2012)</td></tr><tr><td>Alpes sud</td><td>Gurktal</td><td>16-14 ka</td><td>Environnement déglacé</td><td>OSL</td><td>Wölfler et al. (2021)</td></tr><tr><td>Alpes sud</td><td>Alpes Suisses sud</td><td>18,0 ± 0,6 - 17,8 ± 0,6 ka</td><td>Abaissement de la surface de la glace</td><td>Radionucléides cosmogéniques</td><td>Dielforder et Hetzel (2013)</td></tr><tr><td>Alpes nord</td><td>Traun</td><td>19,9-17,7 ka cal BP</td><td>Environnement déglacé</td><td><sup>14</sup>C</td><td>van Husen (1997)</td></tr><tr><td>Alpes nord</td><td>Salzach</td><td>29-21 ka</td><td>Extension LGM 1</td><td>OSL</td><td>Starnberger et al. (2011)</td></tr><tr><td>Alpes nord</td><td>Salzach</td><td>21-20 ka</td><td>Extension LGM 2</td><td>OSL</td><td>Starnberger et al. (2011)</td></tr><tr><td>Alpes nord</td><td>Inn-Chiemsee</td><td>18,7 ± 1,7 ka</td><td>Environnement déglacé</td><td>OSL</td><td>Klasen et al. (2007)</td></tr></tbody></table>
<table><caption>Annexe 2: Table récapitulative des âges utilisés pour la datation absolue des stades glaciaires des glaciers des Alpes occidentales françaises au cours du Pléistocène supérieur. Ces données ont été calibrées en cal ka BP avec la courbe de calibration IntCal20 (Reimer, et al., 2020)</caption><tr><td>Alpes nord</td><td>Isar-Loisach</td><td>18,0 ± 1,9 ka</td><td>Extension maximale</td><td>Radionucléides cosmogéniques</td><td>Reuther et al. (2011)</td></tr><tr><td>Alpes nord</td><td>Rhine</td><td>26,1-25,5 / 27,0-26,0 ka cal BP</td><td>Extension maximale</td><td><sup>14</sup>C</td><td>Preusser et al. (2007)</td></tr><tr><td>Alpes nord</td><td>Rhine</td><td>22,2 ± 1,6 - 17,1 ± 1,3 ka</td><td>Environnement déglacé</td><td>OSL</td><td>Preusser et al. (2007)</td></tr><tr><td>Alpes nord</td><td>Linth</td><td>19,5-18,6 ka cal BP</td><td>Environnement déglacé</td><td><sup>14</sup>C</td><td>Lister (1988)</td></tr><tr><td>Alpes nord</td><td>Reuss (Birrfeld)</td><td>25,1 ± 2,4 - 24,4 ± 2,2 ka</td><td>Extension maximale</td><td>OSL</td><td>Gaar et al. (2019)</td></tr><tr><td>Alpes nord</td><td>Reuss (Lenzburg)</td><td>22,2 ± 1,0 ka</td><td>Etape de récession</td><td>Radionucléides cosmogéniques</td><td>Reber et al. (2014)</td></tr><tr><td>Alpes nord</td><td>Reuss (Lenzburg)</td><td>18,6 ± 0,9 ka</td><td>Environnement déglacé</td><td>Radionucléides cosmogéniques</td><td>Reber et al. (2014)</td></tr><tr><td>Alpes nord</td><td>Aare (Steinhof)</td><td>24,1 ± 1,9 - 22,8 ± 1,8 ka</td><td>Extension maximale</td><td>Radionucléides cosmogéniques</td><td>Gaar et al. (2019)</td></tr><tr><td>Alpes nord</td><td>Aare (Aarwangen)</td><td>27,4 ± 2,8 - 25,7 ± 4,2 ka</td><td>Extension maximale</td><td>OSL</td><td>Preusser et al. (2007)</td></tr><tr><td>Alpes nord</td><td>Aare (Plateau Suisse)</td><td>18,9-18,6 ka cal BP</td><td>Environnement déglacé</td><td><sup>14</sup>C</td><td>Rey et al. (2017)</td></tr><tr><td>Alpes nord</td><td>Rhône (Valais)</td><td>21,9 ± 1,8 ka</td><td>Extension maximale</td><td>Radionucléides cosmogéniques</td><td>Graf et al. (2015)</td></tr><tr><td>Alpes nord</td><td>Alpes Suisses centrale</td><td>23,0 ± 0,8 ka</td><td>Altitude maximum</td><td>Radionucléides cosmogéniques</td><td>Wirsig et al. 2016a</td></tr><tr><td>Alpes nord</td><td>Alpes Suisses centrale</td><td>17,7 ± 0,8 ka</td><td>Abaissement de la surface de la glace</td><td>Radionucléides cosmogéniques</td><td>Wirsig et al. 2016a</td></tr><tr><td>Alpes nord</td><td>Alpes du Zillertal</td><td>18,6 ± 1,4 ka</td><td>Abaissement de la surface de la glace</td><td>Radionucléides cosmogéniques</td><td>Wirsig et al. 2016b</td></tr><tr><td>Alpes ouest</td><td>Rhône (Evian)</td><td>32,3-22,2 ka cal BP</td><td>Extension maximale</td><td><sup>14</sup>C</td><td>Triganon et al. (2005)</td></tr><tr><td>Alpes ouest</td><td>Rhône (Léman ouest)</td><td>23,4-22,4 ka cal BP</td><td>Environnement déglacé</td><td><sup>14</sup>C</td><td>Moscariello et al (1998)</td></tr><tr><td>Alpes ouest</td><td>Romanche</td><td>17,5-13,0 ka</td><td>Environnement déglacé</td><td>Radionucléides cosmogéniques</td><td>Schwartz et al. (2017)</td></tr><tr><td>Alpes ouest</td><td>Durance</td><td>22,0 - 20,9 ka cal BP</td><td>Etape de récession</td><td><sup>14</sup>C</td><td>Jorda et al. (2000)</td></tr><tr><td>Alpes ouest</td><td>Mont Blanc</td><td>18,5 ± 1,1 ka</td><td>Abaissement de la surface de la glace</td><td>Radionucléides cosmogéniques</td><td>Wirsig et al. 2016b</td></tr></table>

<table><caption><sup>14</sup>C</caption><thead><tr><th>Localisation</th><th>N° échantillon</th><th>Lat(°dec)</th><th>Long(°dec)</th><th>Altitude de (m)</th><th>Age ka BP</th><th>Incertitud e ka BP</th><th>Age cal ka BP</th><th>Contexte géologique</th><th>Materiel daté</th><th>Référence</th></tr></thead><tbody><tr><td>Pugnieux</td><td>Ly-2318</td><td>45,8500</td><td>5,1000</td><td>200</td><td>24,11</td><td>0,90</td><td>30,41-26,87</td><td>Dépôt lacustre</td><td>Tourbe</td><td>Evin et al 1985</td></tr><tr><td>Moras</td><td>Lyon-1773(OxA)</td><td>45,6838</td><td>5,2655</td><td>283</td><td>28,16</td><td>0,52</td><td>33,72-31,22</td><td>Dépôt lacustre</td><td>Sédiment riche en MO</td><td>Mandier et al 2003</td></tr><tr><td>Moras</td><td>SacA-12347</td><td>45,6838</td><td>5,2655</td><td>250</td><td>11,34</td><td>0,05</td><td>13,31-13,16</td><td>Dépôt lacustre</td><td>Charbon</td><td>Doyen et al 2015</td></tr><tr><td>Péage-de-Roussillon</td><td>Ly-1689</td><td>45,3428</td><td>4,7882</td><td>140</td><td>14,11</td><td>0,62</td><td>18,77-15,56</td><td>Terrasse fluvial</td><td>Ossement de mamouth</td><td>Chapotat et al 1980</td></tr><tr><td>Chasse</td><td>Ly-653</td><td>45,5835</td><td>4,7832</td><td>158</td><td>14,35</td><td>0,24</td><td>18,20-16,95</td><td>Terrasse fluvial</td><td>Ossement de mamouth</td><td>Evin et al 1975</td></tr><tr><td>Péage-de-Roussillon</td><td>Ly-1690</td><td>45,3533</td><td>4,8004</td><td>135</td><td>20,37</td><td>0,46</td><td>23,56-23,41</td><td>Terrasse fluvial</td><td>Ossement de mamouth</td><td>Chapotat et al 1980</td></tr><tr><td>St Maurice l'Exil</td><td>Ly-360</td><td>45,3958</td><td>4,7750</td><td>155</td><td>18,80</td><td>0,49</td><td>23,88-21,69</td><td>Terrasse fluvial</td><td>Ossement de beuf</td><td>David et al 1972</td></tr><tr><td>Porcieu-Amblagnieu</td><td>Ly-4814</td><td>45,8545</td><td>5,4003</td><td>205</td><td>14,09</td><td>0,12</td><td>17,43-16,77</td><td>Terrasse fluvial</td><td>Ossement de cheval</td><td>Mandier et Pigeay 1991</td></tr><tr><td>Malville</td><td>Ly-3814</td><td>45,7599</td><td>5,4726</td><td>142</td><td>26,47</td><td>0,92</td><td>33,15-28,98</td><td>Dépôt lacustre</td><td>Bois</td><td>Mandier 1988</td></tr><tr><td>St-Hilaire-du-Rosier</td><td>Ly-2629</td><td>45,0693</td><td>5,2568</td><td>200</td><td>15,20</td><td>0,25</td><td>19,00-17,99</td><td>Terrasse fluvial</td><td>Sédiment riche en MO</td><td>Mandier et al 2003</td></tr><tr><td>Cerin</td><td>Ly-5082</td><td>45,7750</td><td>5,5645</td><td>754</td><td>13,68</td><td>0,72</td><td>18,35-14,79</td><td>Dépôt lacustre</td><td>Tourbe</td><td>Bossuet et al 1996</td></tr><tr><td>Annecy</td><td>-</td><td>45,8709</td><td>6,1705</td><td>450</td><td>25,40</td><td>0,17</td><td>30,01-29,24</td><td>Dépôt lacustre</td><td>Sédiment riche en MO</td><td>Manalt 1998</td></tr><tr><td>Grotte de la Garenne</td><td>Ly 702 / OxA 8163</td><td>45,6711</td><td>5,2765</td><td>336</td><td>13,15</td><td>0,18</td><td>16,30-15,26</td><td>Occupation humaine</td><td>Ossement de renne</td><td>Bintz et Evin 2002</td></tr></tbody></table>
<table><tr><td>Grotte des Romains</td><td>Ly-16</td><td>45,7094</td><td>5,7250</td><td>280</td><td>14,38</td><td>0,38</td><td>18,33-16,49</td><td>Occupation humaine</td><td>Charbon</td><td>Loebell 1980</td></tr><tr><td>Paladru</td><td>SacA-29698</td><td>45,4577</td><td>5,3897</td><td>441</td><td>12,02</td><td>0,05</td><td>14,04-13,80</td><td>Dépôt lacustre</td><td>Charbon</td><td>Doyen et al 2015</td></tr><tr><td>Col de la Madeleine</td><td>-</td><td>45,3017</td><td>6,9576</td><td>1675</td><td>7,63</td><td>65,00</td><td>10,52-8,33</td><td>Dépôt lacustre</td><td>Bois</td><td>Couture et al, 1997</td></tr><tr><td>St Julien Mont Denis</td><td>ARC 1764</td><td>45,2602</td><td>6,3874</td><td>555</td><td>9,05</td><td>110,00</td><td>10,51-9,89</td><td>Coulée de débris</td><td>Bois</td><td>Crouzet et al, 1999</td></tr><tr><td>St Julien Mont Denis</td><td>ARC 1775</td><td>45,2602</td><td>6,3874</td><td>552</td><td>8,99</td><td>100,00</td><td>10,38-9,74</td><td>Dépôt fluviatile</td><td>Bois</td><td>Crouzet et al, 1999</td></tr><tr><td>St Julien Mont Denis</td><td>ARC 1349</td><td>45,2515</td><td>6,3960</td><td>658</td><td>7,86</td><td>116,00</td><td>9,00-8,43</td><td>Cône alluviale</td><td>Bois</td><td>Ballandras, 1997</td></tr><tr><td>Pontamafrey</td><td>PON11-1</td><td>45,3166</td><td>6,3490</td><td>738</td><td>10,75</td><td>0,06</td><td>12,79-12,68</td><td>Coulée de débris</td><td>Bois</td><td>Crouzet et al, 2014</td></tr><tr><td>Grottes Jean-Pierre</td><td>Ly-390</td><td>45,5054</td><td>5,8495</td><td>500</td><td>13,30</td><td>0,28</td><td>16,91-15,25</td><td>Occupation humaine</td><td>Charbon</td><td>Bintz et Evin, 2002</td></tr></table>

U/Th

<table><thead><tr><th>Localisation</th><th>N° échantillon</th><th>Lat(°dec)</th><th>Long(°dec)</th><th>Altitu de (m)</th><th>Materiel daté</th><th>Age ka</th><th>Référenc e</th><th></th><th></th></tr></thead><tbody><tr><td rowspan="2">Grotte sous les sangles, Jura sud</td><td>-</td><td>45,8530<br>(entrée)</td><td>5,5405<br>(entrée)</td><td>490</td><td>Spéléothè me</td><td>14,50 ± 2,50</td><td>Lignier et Desmet 2002</td><td></td><td></td></tr><tr><td>-</td><td>45,7387<br>(entrée)</td><td>6,0602<br>(entrée)</td><td>1000</td><td>Spéléothè me</td><td>65</td><td>Jaillet et al 2018</td><td></td><td></td></tr><tr><td>Grotte de Bange, Bauges</td><td>-</td><td>45,7374<br>(entrée)</td><td>6,1021<br>(entrée)</td><td>692</td><td>Spéléothè me</td><td>33-32</td><td>Jaillet et al 2018</td><td></td><td></td></tr></tbody></table>

Age d'exposition ¹⁰Be

<table><caption>Annexe 3: Localisation des données de forages et issues de méthodes géophysiques utilisées pour la reconstitution de la topographie sous-glaciaire.</caption><thead><tr><th>Localisation</th><th>N° échantillon</th><th>Lat(°dec)</th><th>Long(°dec)</th><th>Altitu de (m)</th><th>Materiel daté</th><th>Age ka</th><th>Référenc e</th><th></th><th></th></tr></thead><tbody><tr><td>Combloux-Cordon</td><td>-</td><td>45,9042</td><td>6,6399</td><td>870</td><td>Bloc glaciaire</td><td>17,54 ± 0,50</td><td>Coutterand et Nicoud, 2005</td><td></td><td></td></tr><tr><td rowspan="2">Montsapey</td><td>MSAP12_P1_01</td><td>45,5241</td><td>6,3335</td><td>1040</td><td>Polis glaciaire</td><td>12,82 ± 0,64</td><td>Prud'homme et al, 2020</td><td></td><td></td></tr><tr><td>MSAP12_B1_06</td><td>45,5241</td><td>6,3335</td><td>1040</td><td>Bloc erratique</td><td>15,16 ± 1,85</td><td>Prud'homme et al, 2020</td><td></td><td></td></tr><tr><td>Aussois</td><td>AUSS12_P1_01</td><td>45,2261</td><td>6,7543</td><td>1470</td><td>Polis glaciaire</td><td>11,52 ± 1,75</td><td>Prud'homme et al, 2020</td><td></td><td></td></tr><tr><td>Aussois</td><td>AUSS12_B1_05</td><td>45,2261</td><td>6,7543</td><td>1470</td><td>Bloc erratique</td><td>14,31 ± 0,8</td><td>Prud'homme et al, 2020</td><td></td><td></td></tr><tr><td>Aussois</td><td>AUSS12_B2_06</td><td>45,2261</td><td>6,7543</td><td>1470</td><td>Bloc erratique</td><td>15,19 ± 1,10</td><td>Prud'homme et al, 2020</td><td></td><td></td></tr><tr><td>Aussois</td><td>AUSS12_B3_07</td><td>45,2261</td><td>6,7543</td><td>1470</td><td>Bloc erratique</td><td>13,87 ± 0,88</td><td>Prud'homme et al, 2020</td><td></td><td></td></tr><tr><td>Bessans</td><td>Bessans 05-01</td><td>45,3249</td><td>7,0042</td><td>1735</td><td>Bloc erratique</td><td>11,33 ± 1,06</td><td>Nicoud et al, 2009</td><td></td><td></td></tr><tr><td>Bessans</td><td>Bessans 05-02</td><td>45,3255</td><td>7,0060</td><td>1740</td><td>Bloc erratique</td><td>9,80 ± 0,69</td><td>Nicoud et al, 2009</td><td></td><td></td></tr><tr><td>Bessans</td><td>Bessans 05-03</td><td>45,3234</td><td>7,0075</td><td>1739</td><td>Bloc erratique</td><td>10,07 ± 1,01</td><td>Nicoud et al, 2009</td><td></td><td></td></tr><tr><td>Bessans</td><td>Bessans 05-04</td><td>45,3237</td><td>7,0099</td><td>1742</td><td>Bloc erratique</td><td>10,79 ± 0,79</td><td>Nicoud et al, 2009</td><td></td><td></td></tr><tr><td>Bonneval</td><td>Ev-14a</td><td>45,3243</td><td>7,0074</td><td>1758</td><td>Bloc glaciaire</td><td>12,44 ± 0,67</td><td>Couette et Ghienne, in prep.</td><td></td><td></td></tr><tr><td>Bonneval</td><td>Ev-15</td><td>45,3243</td><td>7,0074</td><td>1758</td><td>Bloc glaciaire</td><td>11,72 ± 0,66</td><td>Couette et Ghienne, in prep.</td><td></td><td></td></tr><tr><td>Bonneval</td><td>Ev-6</td><td>45,3707</td><td>7,1048</td><td>2646</td><td>Poli</td><td>12,86 ± 0,66</td><td>Couette et Ghienne, in prep.</td><td></td><td></td></tr><tr><td>Bonneval</td><td>Ev-8</td><td>45,3707</td><td>7,1037</td><td>2638</td><td>Poli</td><td>13,41 ± 0,70</td><td>Couette et Ghienne, in prep.</td><td></td><td></td></tr></tbody></table>

<table><thead><tr><th>Lat (°dec)</th><th>Long (°dec)</th><th>Altitude substratum (m)</th><th>Methode</th><th>Identifiant</th><th>Source</th></tr></thead><tbody><tr><td>45,2096</td><td>6,5154</td><td>807,9</td><td>Forage</td><td>X10</td><td>Antoine 2014</td></tr><tr><td>45,2106</td><td>6,5142</td><td>795,2</td><td>Forage</td><td>X11</td><td>Antoine 2014</td></tr><tr><td>45,2087</td><td>6,5661</td><td>889,5</td><td>Forage</td><td>XW51</td><td>Antoine 2014</td></tr><tr><td>45,2219</td><td>6,4662</td><td>645</td><td>Géophysique</td><td>03LTF - 01</td><td>Antoine 2014</td></tr><tr><td>45,2198</td><td>6,4651</td><td>550</td><td>Géophysique</td><td>03LTF - 01</td><td>Antoine 2014</td></tr><tr><td>45,5384</td><td>6,3168</td><td>322,9</td><td>Forage</td><td>BSS001VWUL</td><td>BSS</td></tr></tbody></table>
<table><tr><td>45,4607</td><td>6,2945</td><td>348,5</td><td>Forage</td><td>BSS001VWQM</td><td>BSS</td></tr><tr><td>45,2296</td><td>6,4498</td><td>669</td><td>Forage</td><td>BSS001WTGB</td><td>BSS</td></tr><tr><td>45,2095</td><td>6,5178</td><td>798</td><td>Forage</td><td>BSS001WTWE</td><td>BSS</td></tr><tr><td>45,2073</td><td>6,5643</td><td>899</td><td>Forage</td><td>BSS001WTVB</td><td>BSS</td></tr><tr><td>45,2072</td><td>6,5664</td><td>898</td><td>Forage</td><td>BSS001WTVC</td><td>BSS</td></tr><tr><td>45,2036</td><td>6,5820</td><td>921,4</td><td>Forage</td><td>BSS001WUBQ</td><td>BSS</td></tr><tr><td>45,2033</td><td>6,5823</td><td>922</td><td>Forage</td><td>BSS001WUBP</td><td>BSS</td></tr><tr><td>45,2030</td><td>6,5828</td><td>923,3</td><td>Forage</td><td>BSS001WTZL</td><td>BSS</td></tr><tr><td>45,2017</td><td>6,5925</td><td>931,5</td><td>Forage</td><td>BSS001WUAQ</td><td>BSS</td></tr><tr><td>45,1939</td><td>6,6323</td><td>1004,6</td><td>Forage</td><td>BSS001WUAZ</td><td>BSS</td></tr><tr><td>45,1940</td><td>6,6324</td><td>1004</td><td>Forage</td><td>BSS001WUAY</td><td>BSS</td></tr><tr><td>45,1939</td><td>6,6327</td><td>1010,3</td><td>Forage</td><td>BSS001WUAX</td><td>BSS</td></tr><tr><td>45,1938</td><td>6,6327</td><td>1013,2</td><td>Forage</td><td>BSS001WUAW</td><td>BSS</td></tr><tr><td>45,1938</td><td>6,6330</td><td>1017,5</td><td>Forage</td><td>BSS001WUBE</td><td>BSS</td></tr><tr><td>45,1937</td><td>6,6330</td><td>1012</td><td>Forage</td><td>BSS001WUBA</td><td>BSS</td></tr><tr><td>45,1935</td><td>6,6331</td><td>999</td><td>Forage</td><td>BSS001WUBB</td><td>BSS</td></tr><tr><td>45,1938</td><td>6,6332</td><td>1004,4</td><td>Forage</td><td>BSS001WUBG</td><td>BSS</td></tr><tr><td>45,1937</td><td>6,6335</td><td>1008,8</td><td>Forage</td><td>BSS001WUBJ</td><td>BSS</td></tr><tr><td>45,1937</td><td>6,6337</td><td>1014</td><td>Forage</td><td>BSS001WUBL</td><td>BSS</td></tr><tr><td>45,1939</td><td>6,6331</td><td>1017</td><td>Forage</td><td>BSS001WUBD</td><td>BSS</td></tr><tr><td>45,1939</td><td>6,6333</td><td>1018</td><td>Forage</td><td>BSS001WUBF</td><td>BSS</td></tr><tr><td>45,1938</td><td>6,6335</td><td>1019</td><td>Forage</td><td>BSS001WUBH</td><td>BSS</td></tr><tr><td>45,1938</td><td>6,6338</td><td>1019</td><td>Forage</td><td>BSS001WUBK</td><td>BSS</td></tr><tr><td>45,3141</td><td>6,9759</td><td>1631</td><td>Forage</td><td>BSS001WUJJ</td><td>BSS</td></tr><tr><td>45,3189</td><td>6,9986</td><td>1689</td><td>Forage</td><td>BSS001WUJM</td><td>BSS</td></tr><tr><td>45,3217</td><td>7,0048</td><td>1688</td><td>Forage</td><td>BSS001WUJL</td><td>BSS</td></tr><tr><td>45,3210</td><td>6,9934</td><td>1645</td><td>Forage</td><td>BSS001WUKG</td><td>BSS</td></tr><tr><td>45,4258</td><td>6,2748</td><td>361</td><td>Forage</td><td>BSS001VXBT</td><td>BSS</td></tr><tr><td>45,3798</td><td>6,2818</td><td>400</td><td>Forage</td><td>BSS001VXBU</td><td>BSS</td></tr><tr><td>45,3771</td><td>6,2812</td><td>394</td><td>Forage</td><td>BSS001VXCL</td><td>BSS</td></tr><tr><td>45,2959</td><td>6,3539</td><td>500</td><td>Forage</td><td>BSS001WSLS</td><td>BSS</td></tr><tr><td>45,2958</td><td>6,3543</td><td>500</td><td>Forage</td><td>BSS001WSLL</td><td>BSS</td></tr><tr><td>45,2914</td><td>6,3544</td><td>500</td><td>Forage</td><td>BSS001WSJX</td><td>BSS</td></tr><tr><td>45,2904</td><td>6,3619</td><td>505</td><td>Forage</td><td>BSS001WSLJ</td><td>BSS</td></tr><tr><td>45,2848</td><td>6,3620</td><td>499</td><td>Forage</td><td>BSS001WSLV</td><td>BSS</td></tr><tr><td>45,2803</td><td>6,3578</td><td>504</td><td>Forage</td><td>BSS001WSLW</td><td>BSS</td></tr><tr><td>45,2639</td><td>6,3821</td><td>532</td><td>Forage</td><td>BSS001WSVN</td><td>BSS</td></tr><tr><td>45,2552</td><td>6,3982</td><td>507</td><td>Forage</td><td>BSS001WTBG</td><td>BSS</td></tr><tr><td>45,2501</td><td>6,4328</td><td>669</td><td>Forage</td><td>BSS001WTAU</td><td>BSS</td></tr><tr><td>45,2188</td><td>6,4720</td><td>660</td><td>Forage</td><td>BSS001WSZB</td><td>BSS</td></tr><tr><td>45,2093</td><td>6,4766</td><td>714,76</td><td>Forage</td><td>BSS001WSWS</td><td>BSS</td></tr><tr><td>45,2079</td><td>6,5394</td><td>900</td><td>Forage</td><td>BSS001WTWD</td><td>BSS</td></tr><tr><td>45,2055</td><td>6,5720</td><td>902,5</td><td>Forage</td><td>BSS001WUBM</td><td>BSS</td></tr><tr><td>45,2043</td><td>6,5818</td><td>909</td><td>Forage</td><td>BSS001WUBS</td><td>BSS</td></tr></table>
<table><caption>Annexe 4: Synthèse des ELA Dryas récent des glaciers Alpins d'après la synthèse de Baroni et al. (2021) complétée avec les données du stade de Bessans.</caption><tr><td>45,2045</td><td>6,5804</td><td>908</td><td>Forage</td><td>BSS001WUBR</td><td>BSS</td></tr><tr><td>45,2046</td><td>6,5781</td><td>908</td><td>Forage</td><td>BSS001WUBN</td><td>BSS</td></tr><tr><td>45,2043</td><td>6,5763</td><td>920</td><td>Forage</td><td>BSS001WUBU</td><td>BSS</td></tr><tr><td>45,1954</td><td>6,6281</td><td>1000</td><td>Forage</td><td>BSS001WTZN</td><td>BSS</td></tr><tr><td>45,1929</td><td>6,6370</td><td>1034</td><td>Forage</td><td>BSS001WTZQ</td><td>BSS</td></tr><tr><td>45,2531</td><td>6,4242</td><td>630</td><td>Géophysique</td><td></td><td>Crouzet et al 1999</td></tr><tr><td>45,2533</td><td>6,4238</td><td>620</td><td>Géophysique</td><td></td><td>Crouzet et al 1999</td></tr><tr><td>45,2535</td><td>6,4234</td><td>610</td><td>Géophysique</td><td></td><td>Crouzet et al 1999</td></tr><tr><td>45,2538</td><td>6,4231</td><td>600</td><td>Géophysique</td><td></td><td>Crouzet et al 1999</td></tr><tr><td>45,2521</td><td>6,4184</td><td>610</td><td>Géophysique</td><td></td><td>Crouzet et al 1999</td></tr><tr><td>45,2525</td><td>6,4184</td><td>600</td><td>Géophysique</td><td></td><td>Crouzet et al 1999</td></tr><tr><td>45,2527</td><td>6,4183</td><td>590</td><td>Géophysique</td><td></td><td>Crouzet et al 1999</td></tr><tr><td>45,2530</td><td>6,4183</td><td>580</td><td>Géophysique</td><td></td><td>Crouzet et al 1999</td></tr><tr><td>45,2532</td><td>6,4183</td><td>570</td><td>Géophysique</td><td></td><td>Crouzet et al 1999</td></tr><tr><td>45,2548</td><td>6,4178</td><td>570</td><td>Géophysique</td><td></td><td>Crouzet et al 1999</td></tr><tr><td>45,2548</td><td>6,4162</td><td>550</td><td>Géophysique</td><td></td><td>Crouzet et al 1999</td></tr><tr><td>45,2550</td><td>6,4155</td><td>570</td><td>Géophysique</td><td></td><td>Crouzet et al 1999</td></tr><tr><td>45,2545</td><td>6,4135</td><td>540</td><td>Géophysique</td><td></td><td>Crouzet et al 1999</td></tr><tr><td>45,2550</td><td>6,4127</td><td>530</td><td>Géophysique</td><td></td><td>Crouzet et al 1999</td></tr><tr><td>45,2559</td><td>6,4118</td><td>530</td><td>Géophysique</td><td></td><td>Crouzet et al 1999</td></tr><tr><td>45,2561</td><td>6,4115</td><td>550</td><td>Géophysique</td><td></td><td>Crouzet et al 1999</td></tr><tr><td>45,2567</td><td>6,4107</td><td>560</td><td>Géophysique</td><td></td><td>Crouzet et al 1999</td></tr><tr><td>45,2558</td><td>6,4093</td><td>550</td><td>Géophysique</td><td></td><td>Crouzet et al 1999</td></tr><tr><td>45,2528</td><td>6,4089</td><td>470</td><td>Géophysique</td><td></td><td>Crouzet et al 1999</td></tr><tr><td>45,2536</td><td>6,4086</td><td>500</td><td>Géophysique</td><td></td><td>Crouzet et al 1999</td></tr><tr><td>45,2559</td><td>6,4085</td><td>550</td><td>Géophysique</td><td></td><td>Crouzet et al 1999</td></tr><tr><td>45,2547</td><td>6,4083</td><td>540</td><td>Géophysique</td><td></td><td>Crouzet et al 1999</td></tr><tr><td>45,2560</td><td>6,4077</td><td>550</td><td>Géophysique</td><td></td><td>Crouzet et al 1999</td></tr><tr><td>45,2555</td><td>6,4153</td><td>585,8</td><td>Forage</td><td>F41</td><td>Crouzet et al 1999</td></tr><tr><td>45,2602</td><td>6,3929</td><td>522</td><td>Forage</td><td>F62</td><td>Crouzet et al 1999</td></tr><tr><td>45,2563</td><td>6,4073</td><td>595</td><td>Forage</td><td>F35</td><td>Crouzet et al 1999</td></tr><tr><td>45,2578</td><td>6,4042</td><td>625</td><td>Forage</td><td>F51</td><td>Crouzet et al 1999</td></tr><tr><td>45,2588</td><td>6,4027</td><td>662</td><td>Forage</td><td>F3</td><td>Crouzet et al 1999</td></tr><tr><td>45,2574</td><td>6,4028</td><td>633</td><td>Forage</td><td>F4</td><td>Crouzet et al 1999</td></tr><tr><td>45,2589</td><td>6,3956</td><td>609</td><td>Forage</td><td>F61</td><td>Crouzet et al 1999</td></tr><tr><td>45,2596</td><td>6,3953</td><td>593</td><td>Forage</td><td>F2</td><td>Crouzet et al 1999</td></tr><tr><td>45,5605</td><td>6,2502</td><td>37,5</td><td>Géophysique</td><td>Profil 1</td><td>Menard et al 2006</td></tr><tr><td>45,5661</td><td>6,2424</td><td>225</td><td>Géophysique</td><td>Profil 1</td><td>Menard et al 2006</td></tr><tr><td>45,5374</td><td>6,2116</td><td>225</td><td>Géophysique</td><td>Profil 2</td><td>Menard et al 2006</td></tr></table>

<table><thead><tr><td>Localisation</td><td>Pays</td><td>Site</td><td>Longitude E (°dec)</td><td>Latitude N (°dec)</td><td>Méthode</td><td>ELA Dryas récent</td><td>Notes sur le stade Younger Dryas</td><td>Référence</td></tr></thead></table>
<table><tr><td>Schönferwall</td><td>Autriche</td><td>Schönferwall</td><td>10,2</td><td>47,1</td><td>AAR</td><td>2439</td><td>Interprété</td><td>Gross et al. (1977)</td></tr><tr><td>Schönferwall</td><td>Autriche</td><td>Schönferwall</td><td>10,2</td><td>47,1</td><td>AAR</td><td>2320</td><td>Daté</td><td>Sailer (2001) in Baroni et al. (2017)</td></tr><tr><td>Alpes de l'Ötzal</td><td>Autriche</td><td>Vallée de Radurschl</td><td>10,6</td><td>46,9</td><td>AAR</td><td>2610</td><td>Daté</td><td>Moran et al. (2016)</td></tr><tr><td>Alpes de l'Ötzal</td><td>Autriche</td><td>Vallée du Platz</td><td>10,7</td><td>47,0</td><td>AAR</td><td>2590</td><td>Interprété</td><td>Mautner (2012) in Moran et al. (2016)</td></tr><tr><td>Alpes de l'Ötzal</td><td>Autriche</td><td>Kaisenbergtal</td><td>10,7</td><td>46,9</td><td>AAR</td><td>2681</td><td>Interprété</td><td>Gross et al. (1977)</td></tr><tr><td>Alpes de l'Ötzal</td><td>Autriche</td><td>Vallée de Kauner</td><td>10,7</td><td>46,9</td><td>AAR</td><td>2660</td><td>Interprété</td><td>Kerschner (1979)</td></tr><tr><td>Alpes de l'Ötzal</td><td>Autriche</td><td>Kaunertal</td><td>10,7</td><td>47,0</td><td>AAR</td><td>2692</td><td>Interprété</td><td>Gross et al. (1977)</td></tr><tr><td>Alpes de Stubai</td><td>Autriche</td><td>Vallée du Larstig</td><td>11,0</td><td>47,1</td><td>AAR</td><td>2480</td><td>Daté</td><td>Ivy-Ochs et al. (2009)</td></tr><tr><td>Alpes de Stubai</td><td>Autriche</td><td>Vallée du Larstig</td><td>11,0</td><td>47,1</td><td>AAR</td><td>2478</td><td>Interprété</td><td>Gross et al. (1977)</td></tr><tr><td>Alpes de Stubai</td><td>Autriche</td><td>Zwieselbachtal</td><td>11,0</td><td>47,1</td><td>AAR</td><td>2522</td><td>Interprété</td><td>Gross et al. (1977)</td></tr><tr><td>Alpes de Stubai</td><td>Autriche</td><td>Lisenser Laňngental</td><td>11,1</td><td>47,1</td><td>AAR</td><td>2540</td><td>Interprété</td><td>Moran et al. (2017)</td></tr><tr><td>Alpes de Stubai</td><td>Autriche</td><td>Lisenser Laňngental</td><td>11,1</td><td>47,1</td><td>AAR</td><td>2480</td><td>Interprété</td><td>Moran et al. (2017)</td></tr><tr><td>Alpes de Stubai</td><td>Autriche</td><td>Lisenser Laňngental</td><td>11,1</td><td>47,1</td><td>AAR</td><td>2504</td><td>Interprété</td><td>Gross et al. (1977)</td></tr><tr><td>Alpes de Stubai</td><td>Autriche</td><td>Mutterbergtal</td><td>11,2</td><td>47,0</td><td>AAR</td><td>2564</td><td>Interprété</td><td>Gross et al. (1977)</td></tr><tr><td>Alpes de Stubai</td><td>Autriche</td><td>Sulzenau</td><td>11,2</td><td>47,0</td><td>AAR</td><td>2580</td><td>Interprété</td><td>Gross et al. (1977)</td></tr><tr><td>Alpes de Stubai</td><td>Autriche</td><td>Hohes Moos</td><td>11,2</td><td>47,1</td><td>AAR</td><td>2617</td><td>Interprété</td><td>Gross et al. (1977)</td></tr><tr><td>Alpes de Stubai</td><td>Autriche</td><td>Gleirschtal</td><td>11,3</td><td>47,4</td><td>AAR</td><td>2570</td><td>Interprété</td><td>Gross et al. (1977)</td></tr><tr><td>Alpes de Stubai</td><td>Autriche</td><td>Obernbergtal</td><td>11,4</td><td>47,0</td><td>AAR</td><td>2653</td><td>Interprété</td><td>Gross et al. (1977)</td></tr><tr><td>M. Rosa Alps</td><td>Suisse</td><td>Riffelsee</td><td>7,8</td><td>46,0</td><td>AAR</td><td>2750</td><td>Interprété</td><td>Gross et al. (1977)</td></tr><tr><td>Ticino</td><td>Suisse</td><td>Vallée de Bedretto</td><td>8,5</td><td>46,5</td><td>AAR</td><td>2375</td><td>Daté</td><td>Scapozza et al. (2014)</td></tr><tr><td>Vallée de Meien</td><td>Suisse</td><td>Kartigelfirn (Meiental)</td><td>8,5</td><td>46,7</td><td>AAR</td><td>2235</td><td>Daté</td><td>Boxleitner et al. (2019b)</td></tr><tr><td>Vallée de Meien</td><td>Suisse</td><td>Kartigelfirn (Meiental)</td><td>8,5</td><td>46,7</td><td>AAR</td><td>2075</td><td>Daté</td><td>Boxleitner et al. (2019b)</td></tr><tr><td>Vallée de Meien</td><td>Suisse</td><td>Seewenzwachten (Meiental) [MT2]</td><td>8,5</td><td>46,8</td><td>AAR</td><td>2255</td><td>Daté</td><td>Boxleitner et al. (2019b)</td></tr><tr><td>Alpes lépontines</td><td>Suisse</td><td>Alpe Mucia</td><td>9,1</td><td>46,5</td><td>AAR</td><td>2466</td><td>Interprété</td><td>Gross et al. (1977)</td></tr><tr><td>Alpes lépontines</td><td>Suisse</td><td>Hinterrhein</td><td>9,2</td><td>46,5</td><td>AAR</td><td>2392</td><td>Interprété</td><td>Gross et al. (1977)</td></tr><tr><td>Alpes rhétiques ouest</td><td>Suisse</td><td>Val Forno</td><td>9,7</td><td>46,4</td><td>AAR</td><td>2555</td><td>Interprété</td><td>Gross et al. (1977)</td></tr><tr><td>Col Julier</td><td>Suisse</td><td>Col Julier</td><td>9,7</td><td>46,5</td><td>AAR</td><td>2500</td><td>Daté</td><td>Ivy-Ochs et al. (2015)</td></tr><tr><td>Alpes rhétiques ouest</td><td>Suisse</td><td>Val Bever</td><td>9,8</td><td>46,6</td><td>AAR</td><td>2736</td><td>Interprété</td><td>Gross et al. (1977)</td></tr><tr><td>Alpes rhétiques ouest</td><td>Suisse</td><td>Dischmatal</td><td>9,9</td><td>46,8</td><td>AAR</td><td>2516</td><td>Interprété</td><td>Gross et al. (1977)</td></tr><tr><td>Alpes rhétiques ouest</td><td>Suisse</td><td>Val Sartiv</td><td>9,9</td><td>46,7</td><td>AAR</td><td>2619</td><td>Interprété</td><td>Gross et al. (1977)</td></tr><tr><td>Alpes rhétiques ouest</td><td>Suisse</td><td>Val Funtauna</td><td>9,9</td><td>46,7</td><td>AAR</td><td>2585</td><td>Interprété</td><td>Gross et al. (1977)</td></tr><tr><td>Massifs des Ecrins / Ceres</td><td>France</td><td>Vallée de Prelles</td><td>6,3</td><td>44,7</td><td>AAR</td><td>2372</td><td>Daté</td><td>Hofmann et al. (2019)</td></tr><tr><td>Massifs des Ecrins / Ceres</td><td>France</td><td>Vallée de Rougnoux</td><td>6,3</td><td>44,8</td><td>AAR</td><td>2218</td><td>Daté</td><td>Hofmann et al. (2019)</td></tr><tr><td>Massifs des Ecrins / Ceres</td><td>France</td><td>Vallée de la Clarée</td><td>6,7</td><td>45,0</td><td>THA R</td><td>2343</td><td>Daté</td><td>Cossart et al. (2012)</td></tr><tr><td>Massif du Mont Blanc</td><td>France</td><td>Glacier de l'Argentiere</td><td>7,0</td><td>45,9</td><td>AAR</td><td>2648</td><td>Daté</td><td>Protin et al. (2019)</td></tr><tr><td>Massif du Mont Blanc</td><td>France</td><td>Glacier de l'Argentiere</td><td>7,0</td><td>45,9</td><td>AAB R</td><td>2523</td><td>Daté</td><td>Protin et al. (2019)</td></tr><tr><td>Maurienne</td><td>France</td><td>Bessans</td><td>7,0</td><td>45,3</td><td>AAR</td><td>2697</td><td>Daté</td><td>Cette étude</td></tr><tr><td>Maurienne</td><td>France</td><td>Bessans</td><td>7,0</td><td>45,3</td><td>AAB R</td><td>2747</td><td>Daté</td><td>Cette étude</td></tr><tr><td>Massif du Mont Blanc</td><td>Italie</td><td>Monte Bianco</td><td>6,9</td><td>45,8</td><td>AAR</td><td>2450</td><td>Interprété</td><td>Porter & Orombelli (1982), Vanuzzo (2001)</td></tr><tr><td>Alpes maritimes</td><td>Italie</td><td>Forneris Glacier (Stura)</td><td>6,9</td><td>44,4</td><td>AAB R</td><td>2349</td><td>Daté</td><td>Spagnolo & Ribolini (2019)</td></tr><tr><td>Alpes maritimes</td><td>Italie</td><td>Piano del Praiet</td><td>7,4</td><td>44,1</td><td>AAB R</td><td>2368</td><td>Daté</td><td>Federici et al. (2017)</td></tr><tr><td>Alpes maritimes</td><td>Italie</td><td>Piano del Praiet</td><td>7,4</td><td>44,1</td><td>AAR</td><td>2305</td><td>Daté</td><td>Federici et al. (2017)</td></tr><tr><td>Alpes maritimes</td><td>Italie</td><td>Peirastretta</td><td>7,4</td><td>44,1</td><td>AAR</td><td>2207</td><td>Daté</td><td>Federici et al. (2017)</td></tr><tr><td>Alpes maritimes</td><td>Italie</td><td>Peirastretta</td><td>7,4</td><td>44,1</td><td>AAB R</td><td>2217</td><td>Daté</td><td>Federici et al. (2017)</td></tr></table>
<table><caption>Annexe 5: Synthèse des bilans de masse de glacier alpins actuels entre la fin du 19ème et le 21ème siècle.</caption><tr><td>Alpes rhétiques ouest</td><td>Italie</td><td>Val Viola</td><td>10,2</td><td>46,4</td><td></td><td>2140</td><td>Daté</td><td>Hormes et al. (2008)</td></tr><tr><td>Alpes rhétiques ouest</td><td>Italie</td><td>Vallée de Dosdè</td><td>10,2</td><td>46,4</td><td>AAR</td><td>2649</td><td>Daté</td><td>Scotti et al. (2017)</td></tr><tr><td>Alpes rhétiques ouest</td><td>Italie</td><td>Vallée de Dosdè</td><td>10,2</td><td>46,4</td><td>AAB R</td><td>2689</td><td>Daté</td><td>Scotti et al. (2017)</td></tr><tr><td>Alpes rhétiques ouest</td><td>Italie</td><td>Vallée de Dosdè</td><td>10,2</td><td>46,4</td><td>AAR</td><td>2619</td><td>Daté</td><td>Scotti et al. (2017)</td></tr><tr><td>Alpes rhétiques ouest</td><td>Italie</td><td>Vallée de Dosdè</td><td>10,2</td><td>46,4</td><td>AAB R</td><td>2659</td><td>Daté</td><td>Scotti et al. (2017)</td></tr><tr><td>Alpes rhétiques sud</td><td>Italie</td><td>Glacier de La Mare</td><td>10,6</td><td>46,4</td><td>AAR</td><td>2825</td><td>Daté</td><td>Baroni et al. (2017)</td></tr><tr><td>Alpes de l'Ötzal</td><td>Italie</td><td>Vallée de Langtaufers</td><td>10,7</td><td>46,8</td><td>AAR</td><td>2650</td><td>Daté</td><td>Moran et al. (2016)</td></tr><tr><td>Alpes rhétiques sud</td><td>Italie</td><td>Careser Glacier</td><td>10,7</td><td>46,5</td><td>AAR</td><td>2845</td><td>Daté</td><td>Baroni et al. (2017), Carturan &amp; Seppi (2007)</td></tr><tr><td>Groupe du Grand Paradis</td><td>Italie</td><td>Vallée de Rhèmes</td><td>7,1</td><td>45,6</td><td>AAR</td><td>2565</td><td>Daté</td><td>Baroni et al. (2021)</td></tr><tr><td>Groupe du Grand Paradis</td><td>Italie</td><td>Vallée de Rhèmes</td><td>7,1</td><td>45,6</td><td>AAB R</td><td>2630</td><td>Daté</td><td>Baroni et al. (2021)</td></tr><tr><td>Groupe du Grand Paradis</td><td>Italie</td><td>Valsavarenche</td><td>7,2</td><td>45,6</td><td>AAR</td><td>2745</td><td>Daté</td><td>Baroni et al. (2021)</td></tr><tr><td>Groupe du Grand Paradis</td><td>Italie</td><td>Valsavarenche</td><td>7,2</td><td>45,6</td><td>AAB R</td><td>2750</td><td>Daté</td><td>Baroni et al. (2021)</td></tr><tr><td>Groupe du Grand Paradis</td><td>Italie</td><td>Valnontey</td><td>7,3</td><td>45,6</td><td>AAR</td><td>2985</td><td>Daté</td><td>Baroni et al. (2021)</td></tr><tr><td>Groupe du Grand Paradis</td><td>Italie</td><td>Valnontey</td><td>7,3</td><td>45,6</td><td>AAB R</td><td>2970</td><td>Daté</td><td>Baroni et al. (2021)</td></tr><tr><td>Groupe du Grand Paradis</td><td>Italie</td><td>Grivola</td><td>7,3</td><td>45,6</td><td>AAR</td><td>2465</td><td>Daté</td><td>Baroni et al. (2021)</td></tr><tr><td>Groupe du Grand Paradis</td><td>Italie</td><td>Grivola</td><td>7,3</td><td>45,6</td><td>AAB R</td><td>2500</td><td>Daté</td><td>Baroni et al. (2021)</td></tr><tr><td>Groupe du Grand Paradis</td><td>Italie</td><td>Vaveille</td><td>7,4</td><td>45,6</td><td>AAR</td><td>2725</td><td>Daté</td><td>Baroni et al. (2021)</td></tr><tr><td>Groupe du Grand Paradis</td><td>Italie</td><td>Vaveille</td><td>7,4</td><td>45,6</td><td>AAB R</td><td>2740</td><td>Daté</td><td>Baroni et al. (2021)</td></tr><tr><td>Groupe du Grand Paradis</td><td>Italie</td><td>Vallée d'Orco</td><td>7,3</td><td>45,5</td><td>AAR</td><td>2755</td><td>Daté</td><td>Baroni et al. (2021)</td></tr><tr><td>Groupe du Grand Paradis</td><td>Italie</td><td>Vallée d'Orco</td><td>7,3</td><td>45,5</td><td>AAB R</td><td>2775</td><td>Daté</td><td>Baroni et al. (2021)</td></tr><tr><td>Alpes juliennes</td><td>Slovénie</td><td>Vallée de Krnica</td><td>13,8</td><td>46,5</td><td>AAR</td><td>1812</td><td>Interprété</td><td>Kozamernik et al. (2018)</td></tr></table>

<table><thead><tr><th>Localisation</th><th>Période étudiée</th><th>Méthode</th><th>Référence</th><th>Bilan de masse (m eq e. an-1)</th></tr></thead><tbody><tr><td>Alpes</td><td>1850-1970</td><td>Relevés topographiques</td><td>Hoelzle et al., 2007</td><td>-0,33</td></tr><tr><td>Alpes</td><td>2000-2016</td><td>Télédétection</td><td>Dazave et al., 2020</td><td>-0,74 ± 0,20</td></tr><tr><td>Alpes</td><td>1983-2002 / 2003-2013</td><td>Mesures in situ</td><td>Vincent et al., 2017</td><td>-0,85 (1983-2002), -1,63 (2003-2013)</td></tr><tr><td>Alpes</td><td>1979-2011</td><td>Télédétection</td><td>Rabatel et al., 2016</td><td>-0,66 ± 0,27</td></tr><tr><td>Alpes</td><td>1900-2011</td><td>Extrapolation de mesures de bilans de masse</td><td>Huss, 2012</td><td>-0,31 ± 0,04</td></tr><tr><td>Alpes</td><td>1973-1998</td><td>Télédétection</td><td>Paul et al., 2004</td><td>-0,36</td></tr><tr><td>Alpes</td><td>1975-2000</td><td>Mesures in situ, télédétection, modélisation</td><td>Zemp et al., 2006</td><td>-0,5</td></tr><tr><td>Alpes Suisses</td><td>1870-2004</td><td>Télédétection et relevés topographiques</td><td>Bauder et al., 2007</td><td>-0,29 (1920-60), -0,03 (1960-80), -0,53 (1980-2004)</td></tr><tr><td>Alpes Suisses</td><td>1980-2010</td><td>Analyse de MNT</td><td>Fischer et al., 2015</td><td>-0,62 ± 0,03</td></tr></tbody></table>