[PDF] Correction: Dupuy, E, et al Comparison of XH2O Retrieved

The Napoleon Series

The battery joined the regiment on the 15th of September, at Orléans, and the contingent thus assembled reached Irun on the evening of the 31st, after having receiving at Bayonne camp utensils, provisions, and a complement of ammunition The German division was organized in Durango

University of Groningen TCCON and NDACC XCO measurements Zhou

regular AirCore measurements at Orléans and Sodankylä are compared to co-located TCCON measurements It is found that TCCON XCO measurements are 6 1 1 6 and 8 0 3 2 smaller than the AirCore measurements at Orléans and Sodankylä, respectively, indicating that the scaling fac-tor of TCCON XCO data should be around 1 0000 instead of 1 0672

Retrieval of atmospheric CH vertical information from ground

Sodankylä, Bialystok, Bremen, Orléans and St Denis) for measurements performed during the time period of 2016– 2017 in the framework of the EU Readiness of ICOS for Ne-cessities of integrated Global Observations (RINGO) project The full-physics SFIT4 retrieval code is based on the opti-mal estimation method (Rodgers,2000), which is an updated

Correction: Dupuy, E, et al Comparison of XH2O Retrieved

Water vapour Isotopologues from TROPOMI (WIFT)

Orléans Ga h P alls Rikub tsu Lamont T sukuba Edw rds JPL P adena Saga Burgos W ng Lauder 100 80 60 40 20 0 20 Rigel Kivi, Frank Hase, Matthias Schneider, and

Contributions of the troposphere and stratosphere to CH model

Orléans 47 97 2 113 130 Messerschmidt et al (2010) Garmisch 47 476 11 063 740 Sussmann et al (2013), Sussmann and Rettinger (2014) Park Falls 45 945 90 273 440 Washenfelder et al (2006) Lamont 36 604 97 486 320 Wunch et al (2009) Izaña 28 3 16 483 2370 Blumenstock et al (2014) Darwin 12 424 130 891 30 Deutscher et al (2010)

Specification for high accuracy in situ vertical profile

performed during the RINGO campaigns at Sodankylä, Finland and Orléans, France to the AirCore measurements from the different groups The difference was found to be within the uncertainty estimates of the SFIT4NIR results The small differences among the AirCore results are better understood Our method to retrieve CH

Evaluation of Bias Correction Methods for GOSAT SWIR XH O

Thorsten Warneke 3, Christof Petri 3, Rigel Kivi 4, Frank Hase 5, David F Pollard 6, Nicholas M Deutscher 7, Voltaire A Velazco 7, Laura T Iraci 8, James R Podolske 8 and Manvendra K Dubey 9 1 Satellite Observation Center, National Institute for Environmental Studies (NIES), 16-2 Onogawa,

Loi de Wien - Académie dOrléans-Tours

5 On donne les valeurs de l’émittance M* (issues de mesures expérimentales) pour différentes longueurs d’onde λ λ (m) 300 320 340 360 370 380 390 400 410 420 430

Actes CGénial 2018 - Académie dOrléans-Tours

3 Finale Académique - Orléans-Tours – C Génial Collège Campus du CNRS d’Orléans le 4 avril 2018 SOMMAIRE 1 Construire une maison écologique (Collège F Bazille – Beaune la Rolande – 45) 4 2 La lumière, le messager des étoiles (Collège Voltaire – St Florent sur Cher – 18) 5