Reflectance spectra of subarctic lichens

Abstract Lichens constitute a major portion of the ground cover of high latitude environments, but little has been reported concerning their in situ solar spectral reflectance properties. Knowledge of these properties is important for the interpretation of remotely sensed observations from high latitude regions, as well as in studies of high latitude ecology and energy balance climatology. The spectral reflectance of common boreal vascular plants is similar to that of vascular plants of the midlatitudes. The dominant lichens, in contrast, display variable reflectance patterns in visible wavelengths. The relative reflectance peak at 0.55 μm, common to green vegetation, is absent or indistinct in spectra of pervasive boreal forest and tundra lichens, despite the presence of chlorophyll in the inner algal cells. Lichens of the dominant genus, Cladina , display strong absorption of ultraviolet energy and short-wavelength blue light relative to their absorption in other visible wavelengths. Since the Cladinae dominate both the surface vegetation in open woodlands of the boreal forest and the low arctic tundra, their unusual spectral reflectance patterns will enable accurate monitoring of the boreal forest-tundra ecotone and detection of its vigor and movement in the future.

[1]  David H. S. Richardson,et al.  The vanishing lichens: Their history, biology and importance , 1975 .

[2]  D. N. Rao,et al.  A Possible Role of Atranorin in the Lichen Thallus , 1965 .

[3]  G. Asrar,et al.  Estimating Absorbed Photosynthetic Radiation and Leaf Area Index from Spectral Reflectance in Wheat1 , 1984 .

[4]  Giannino Laudi,et al.  Differenze Ultrastrutturali Di Alcune Specie Di Trebouxia Poste in Condizioni Di Illuminazione Differenti , 1969 .

[5]  A F Goetz,et al.  Imaging Spectrometry for Earth Remote Sensing , 1985, Science.

[6]  Mason E. Hale,et al.  The Biology of Lichens , 1969 .

[7]  Dieter Steiner,et al.  Russian data on spectral reflectance of vegetation, soil and rock types : final technical report , 1966 .

[8]  D. E. Petzold,et al.  Vegetation Distributions along Lichen-Dominated Slopes of Opposing Aspect in the Eastern Canadian Subarctic , 1987 .

[9]  M. Caldwell,et al.  A STEEP LATITUDINAL GRADIENT OF SOLAR ULTRAVIOLET-B RADIATION IN THE ARCTIC-ALPINE LIFE ZONE' , 1980 .

[10]  W. Oechel,et al.  Effects of Several Microclimatic Factors and Nutrients on Net Carbon Dioxide Exchange in Cladonia alpestris (L.) Rabh. in the Subarctic , 1978 .

[11]  J. Hansen,et al.  Climate Impact of Increasing Atmospheric Carbon Dioxide , 1981, Science.

[12]  A. Rencz,et al.  The Albedo of Selected Subarctic Surfaces , 1975 .

[13]  Philip H. Swain,et al.  Remote Sensing: The Quantitative Approach , 1981, IEEE Transactions on Pattern Analysis and Machine Intelligence.

[14]  Melvin B. Satterwhite,et al.  Effects of lichens on the reflectance spectra of granitic rock surfaces , 1985 .