Sie haben gesucht nach VerfasserIn: 'Falourd, S.', in der Datenbank: Bibliothekskatalog.
Anzahl der Treffer: 4
|
|
|
| 1 |
|
 |
 |
Links between MIS 11 millennial to sub-millennial climate variability and long term trends as revealed by new high resolution EPICA Dome C deuterium data – A comparison with the Holocene
Pol, K.; Debret, M.; Masson-Delmotte, V.; Capron, E.; Cattani, O.; Dreyfus, G.; Falourd, S.; Johnsen, S.; Jouzel, J.; Landais, A.; Minster, B.; Stenni, B.
In: Climate of the Past ; 7, no. 2
|
2011
|
| 2 |
|
|
|
Continuous monitoring of summer surface water vapor isotopic composition above the Greenland Ice Sheet
Steen-Larsen, H. C.; Johnsen, S. J.; Masson-Delmotte, V.; Stenni, B.; Risi, C.; Sodemann, H.; Balslev-Clausen, D.; Blunier, T.; Dahl-Jensen, D.; Ellehøj, M. D.; Falourd, S.; Grindsted, A.; Gkinis, V.; Jouzel, J.; Popp, T.; Sheldon, S.; Simonsen, S. B.; Sjolte, J.; Steffensen, J. P.; Sperlich, P.; Sveinbjörnsdóttir, Á. E.; Vinther, B. M.; White, J. W. C.
In: Atmospheric Chemistry and Physics ; 13, no. 9
|
2013
|
| 3 |
|
|
|
Recent changes in north-west Greenland climate documented by NEEM shallow ice core data and simulations, and implications for past-temperature reconstructions
Masson-Delmotte, V.; Steen-Larsen, H. C.; Ortega, P.; Swingedouw, D.; Popp, T.; Vinther, B. M.; Oerter, H.; Sveinbjörnsdóttir, Á. E.; Gudlaugsdottir, H.; Box, J. E.; Falourd, S.; Fettweis, X.; Gallée, H.; Garnier, E.; Gkinis, V.; Jouzel, J.; Landais, A.; Minster, B.; Paradis, N.; Orsi, A.; Risi, C.; Werner, M.; White, J. W. C.
In: The Cryosphere ; 9, no. 4
|
2015
|
| 4 |
|
|
|
Evidence for a three-phase sequence during Heinrich Stadial 4 using a multiproxy approach based on Greenland ice core records
Guillevic, M.; Bazin, L.; Landais, A.; Stowasser, C.; Masson-Delmotte, V.; Blunier, T.; Eynaud, F.; Falourd, S.; Michel, E.; Minster, B.; Popp, T.; Prié, F.; Vinther, B. M.
In: Climate of the Past ; 10, no. 6
|
2014
|
Sie haben gesucht nach VerfasserIn: 'Falourd, S.', in der Datenbank: Bibliothekskatalog.
Anzahl der Treffer: 4
|
|
|
|