1 / 1

spectrolinoplusspektren

The analysis of spectral features (absorption bands, continuum) in the reflectance spectra is described in REIN, B. & F. SIROCKO ( 2002 ): In-situ reflectance spectroscopy – Analyzing techniques for high resolution pigment logging in sediment cores.

pearlie-kyrie
Télécharger la présentation

spectrolinoplusspektren

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript

  1. The analysis of spectral features (absorption bands, continuum) in the reflectance spectra is described in REIN, B. &F. SIROCKO (2002): In-situ reflectance spectroscopy – Analyzing techniques for high resolution pigment logging in sediment cores. Int. J. Earth Sci. (GR), 91: 950-954, DOI: 10.1007/s00531-002-0264-0. Erratum (2003): 92: 143, DOI: 10.1007/s00531-002-0308-5. [PDFmailto:brein@uni-mainz.de]. REIN, B. &F. SIROCKO (2002): In-situ Reflektionsspektroskopie zur Rekonstruktion von Paläoklima und Paläozeanographie am Beispiel El Niños. Publ. Dt. Ges. Photogrammetrie u. Fernerkundung, 11: 227-235. [Abstract] [PDFmailto:brein@uni-mainz.de] REIN, B., A. LÜCKGE & F. SIROCKO (2004): A major Holocene ENSO anomaly during the Medieval period. Geophysical Research Letters, 31: L17211, doi:10.1029/2004GL020161. [PDF incl. supplementary material mailto:brein@uni-mainz.de][Data]. The quantification of these results is described in REIN, B., A. LÜCKGE, R. LUTZ, F. SIROCKO, A.WOLF, C-W. DULLO (2005): El Niño variability off Peru during the last 20,000 years. Paleoceanography, 20, PA4003 (1-17), doi:10.1029/2004PA001099. [PDFmailto:brein@uni-mainz.de] [Data]

More Related