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More than a decade has passed since Professor Gisela Jahn completed
Volume 12 of the Handbook of Vegetation Science, dealing with the
application of vegetation science in forestry, mostly European
forestry. The volume was well received by the critics with the
exception that they wanted a more diversified demonstration of
forestry-related vegetation science work and a wider representation
of forest types from different continents. The topics covered in
this volume, 12/1, widen the scope of vegetation science work in
forestry over the phytosociological work which was the main focus
in the Handbook as perceived by Dr Tuxen. Section 1. Overview T.
Kira: Forest Ecosystems of East and Southeast Asia in a Global
Perspective; E.O. Box: Climatic Relations of the Forests of East
and Southeast Asia; K. Iwatsuki: Species Diversity in East Asia in
Global Perspective. The remaining contributions are divided into
the following sections: Evergreen Forest Region; Summergreen Forest
Region; Montane/Boreal Region; Tropical Forest Region. "
This study arose out ofthe old question of what actually determines
vegetation structure and distributions. Is climate the overriding
control, as one would suppose from reading the more geographically
oriented literature? Or is climate only incidental, as suggested by
more site and/ or taxon-oriented writers? The question might be
phrased more realistically: How much does climate control
vegetation processes, structures, and distributions? It seemed to
me, as an ambitious doctoral student, that one way to attempt an
answer might be to try to predict world vegetation from climate
alone and then compare the predicted results with actual vegetation
patterns. If climatic data were sufficient to reproduce the world's
actual vegetation patterns, then one could conclude that climate is
the main control. This book represents an expanded,
second-generation version of that original thesis. It presents
world-scale vegetation and ecoclimatic models and a methodology for
applying such models to predict vegetation and for evaluating model
results. This approach also provides a means of geographical
simulation of vegetation patterns and changes, which represent
necessary data inputs in other fields such as atmospheric chemistry
and biogeochemical cycling. It has been fairly well accepted that
climatic and other environmental conditions are associated with the
evolution of particular aspects of plant form (convergent
evolution). The particular configurations of plant size,
photosynthetic surface area and structure (e. g. sclerophylly,
stomatal 'resistance'), and their seasonal variations represent
what one can recognize fairly readily as distinct growth forms.
This study arose out ofthe old question of what actually determines
vegetation structure and distributions. Is climate the overriding
control, as one would suppose from reading the more geographically
oriented literature? Or is climate only incidental, as suggested by
more site and/ or taxon-oriented writers? The question might be
phrased more realistically: How much does climate control
vegetation processes, structures, and distributions? It seemed to
me, as an ambitious doctoral student, that one way to attempt an
answer might be to try to predict world vegetation from climate
alone and then compare the predicted results with actual vegetation
patterns. If climatic data were sufficient to reproduce the world's
actual vegetation patterns, then one could conclude that climate is
the main control. This book represents an expanded,
second-generation version of that original thesis. It presents
world-scale vegetation and ecoclimatic models and a methodology for
applying such models to predict vegetation and for evaluating model
results. This approach also provides a means of geographical
simulation of vegetation patterns and changes, which represent
necessary data inputs in other fields such as atmospheric chemistry
and biogeochemical cycling. It has been fairly well accepted that
climatic and other environmental conditions are associated with the
evolution of particular aspects of plant form (convergent
evolution). The particular configurations of plant size,
photosynthetic surface area and structure (e. g. sclerophylly,
stomatal 'resistance'), and their seasonal variations represent
what one can recognize fairly readily as distinct growth forms.
Landscape pattern is generated by a variety of processes, including
disturbances. In turn, the heterogeneity of the landscape may
enhance or retard the spread of disturbance. The complex
relationship between landscape pattern and disturbance is the
subject of this book. It is designed to present an illustrative
analysis of the topic, presenting the perspectives of several
different disciplines. The book includes conceptual considerations,
empirical studies, and management examples. Important features
include: hypotheses about the spread of disturbance and the effects
of scale changes in landscape studies; the multidisciplinary
approach; and the explicit focus on the landscape level. The
intended audience comprises graduate students, academics, and
professionals interested in landscape ecology. The reader will
receive a state-of-the-art treatment of a current topic in
landscape ecology.
More than a decade has passed since Professor Gisela Jahn completed
Volume 12 of the Handbook of Vegetation Science, dealing with the
application of vegetation science in forestry, mostly European
forestry. The volume was well received by the critics with the
exception that they wanted a more diversified demonstration of
forestry-related vegetation science work and a wider representation
of forest types from different continents. The topics covered in
this volume, 12/1, widen the scope of vegetation science work in
forestry over the phytosociological work which was the main focus
in the Handbook as perceived by Dr Tuxen. Section 1. Overview T.
Kira: Forest Ecosystems of East and Southeast Asia in a Global
Perspective; E.O. Box: Climatic Relations of the Forests of East
and Southeast Asia; K. Iwatsuki: Species Diversity in East Asia in
Global Perspective. The remaining contributions are divided into
the following sections: Evergreen Forest Region; Summergreen Forest
Region; Montane/Boreal Region; Tropical Forest Region. "
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