All rights reserved. No part of this periodical may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopying, recording, or any information storage and retrieval system, without permission in writing from the publisher. Permission for printing and for reprinting the material contained herein has been obtained by the publisher. Spectral indices (SI) derived from crop refl ectance data are sensitive to chlorophyll a and b content (Chl). However, the SI-Chl relationship might be confounded by variation in leaf area index (LAI) and soil background refl ectance, especially in semiarid environments where water determines crop growth. Th is study evaluated the sensitivity of SI to variation in soil refl ectance and how this may aff ect overall SI performance for ground-based sensing of Chl in dryland wheat (Triticum aestivum L.). Selected SI were computed from spectra simulated by the PROSPECT-SAIL radiative-transfer model for 5 LAI values, 7 Chl values, and 121 dry soil surface refl ectance spectra. Th ese spectra represented soils across major wheat growing areas in the United States. Soil properties and refl ectance varied widely among the soils indicated by the high SI variation for LAI values < 1.5. Overall, soil background variation contributed less to the observed SI variability (<6%) than LAI (<97%). Combined indices [i.e., Normalized Diff erence Red Edge Index (NDRE)/Normalized Diff erence Vegetation Index (NDVI) and Modifi ed Chlorophyll Absorption Ratio Index (MCARI)/Second Modifi ed Triangular Vegetation Index (MTVI)] were least aff ected by soil background variation than single indices (i.e., NDVI). Results showed that ground sensing of Chl may be improved by means of combined indices that are resistant to soil background and LAI. Empirical measurements verifi ed that the modeling results were a reliable representation of the infl uence of Chl, LAI, and soil on canopy refl ectance. Further research is needed to evaluate the eff ect of soil moisture, surface roughness, residue, growth stage, and shadow on SI. Abbreviations: Chl, chlorophyll a and b content; GESAVI, Generalized soil adjusted vegetation index; LAI, leaf area index; MCARI, modifi ed chlorophyll absorption in refl ective index; NDRE, normalized diff erence red edge index; NDVI, normalized diff erence vegetation index; OSAVI, optimized soil adjusted vegetation index; SAVI, Soil Adjusted Vegetation Index; SI spectral index; MTV2, Second Modifi ed Triangular Vegetation Index; TCARI, transformed chlorophyll absorption in refl ectance index; TSAVI, Transformed Soil Adjusted Vegetation Index.