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Vegetation-Climate Interaction: How Plants Make the Global Environment Second Edition 2010 [Hardback]

  • Formāts: Hardback, 266 pages, height x width: 244x170 mm, weight: 702 g, XXVII, 266 p., 1 Hardback
  • Sērija : Environmental Sciences
  • Izdošanas datums: 31-Aug-2009
  • Izdevniecība: Springer-Verlag Berlin and Heidelberg GmbH & Co. K
  • ISBN-10: 3642008801
  • ISBN-13: 9783642008801
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  • Formāts: Hardback, 266 pages, height x width: 244x170 mm, weight: 702 g, XXVII, 266 p., 1 Hardback
  • Sērija : Environmental Sciences
  • Izdošanas datums: 31-Aug-2009
  • Izdevniecība: Springer-Verlag Berlin and Heidelberg GmbH & Co. K
  • ISBN-10: 3642008801
  • ISBN-13: 9783642008801
Citas grāmatas par šo tēmu:
This book offers a readable and accessible account of the way in which the world's plant life partly controls its own environment. Starting from the broad patterns in vegetation which have classically been seen as a passive response to climate, the authors build up from the local scale - with microclimates produced by plants - to the regional and global scale. The influence of plants (both on land and in the ocean) in making clouds, haze and rain are considered, along with plant effects on the composition of greenhouse gases in the earth's atmosphere. Broad global feedbacks that either stabilize or destabilize the earth's environment will be explored, in the context of environmental change in the recent geological past, and in the near future. Common contentions and misconceptions about the role of vegetation or forest removal in the spread of deserts will also be considered.

Recenzijas

From the reviews:









"Vegetation-Climate Interaction is a wonderfully simple yet elegant treatise on how vegetation patterns are closely linked to the global environment. The book is liberally laced with useful figures and photos that contribute greatly to making the complex topics understandable. All in all, this volume is likely to become a staple for both the vegetation and climate change communities, and for meteorologically oriented scientists. It would be a perfect primer for qualifier exams in these fields. Summing Up: Highly recommended. All levels." (D. F. Karnosky, CHOICE, Vol. v4 (3), November, 2007)

Preface to the Second Edition xi
Preface to the First Edition xiii
Foreword xv
List of figures
xvii
List of tables
xxiii
List of abbreviations and acronyms
xxv
About the author xxvii
The climate system
1(26)
Why does climate vary from one place to another?
2(4)
Why mountains are colder
4(2)
Winds and currents: the atmosphere and oceans
6(3)
The ocean circulation
9(1)
Ocean gyres and the ``Roaring Forties'' (or Furious Fifties)
9(1)
Winds and ocean currents push against one another
10(1)
The thermohaline circulation
10(5)
The great heat-transporting machine
15(12)
The ``continental'' climate
17(1)
Patterns of precipitation
18(9)
From climate to vegetation
27(40)
Biomes: the broad vegetation types of the world
27(1)
An example of a biome or broad-scale vegetation type: tropical rainforest
28(3)
The world's major vegetation types
31(6)
Understanding the patterns
37(2)
What favors forest vegetation
39(4)
Why trees need more warmth
39(1)
Why trees need more water
40(3)
Deciduous or evergreen: the adaptive choices that plants make
43(5)
Cold-climate evergreenness
48(2)
The latitudinal bands of evergreen and deciduous forest
50(1)
Nutrients and evergreenness
50(2)
Other trends in forest with climate
52(1)
Non-forest biomes
53(1)
Scrub biomes
53(1)
Grasslands
53(1)
Deserts
54(1)
Biomes are to some extent subjective
54(1)
Humans altering the natural vegetation, shifting biomes
55(1)
``Predicting'' where vegetation types will occur
55(4)
Species distributions and climate
59(8)
Patterns in species richness
60(7)
Plants on the move
67(30)
Vegetation can move as the climate shifts
67(1)
The Quaternary: the last 2.4 million years
67(8)
Biomes in the distant past
75(6)
Sudden changes in climate, and how vegetation responds
75(6)
The increasing greenhouse effect, and future vegetation change
81(1)
Response of vegetation to the present warming of climate
81(5)
Seasons as well as vegetation distribution are changing
86(2)
What will happen as the warming continues?
88(9)
Movement of biomes under greenhouse effect warming
92(5)
Microclimates and vegetation
97(24)
What causes microclimates?
97(20)
At the soil surface and below
98(1)
Above the surface: the boundary layer and wind speed
99(3)
Roughness and turbulence
102(1)
Microclimates of a forest canopy
103(3)
Under the canopy
106(2)
Big plants ``make'' the microclimates of smaller plants
108(2)
The importance of sun angle
110(2)
Bumps and hollows in the landscape have their own microclimate
112(2)
Life within rocks: endolithic lichens and algae
114(1)
Plants creating their own microclimate
115(1)
Dark colors
115(1)
Protection against freezing
115(1)
Internal heating
115(1)
Volatiles from leaves
116(1)
Utilization of microclimates in agriculture
116(1)
From microclimates to macroclimates
117(4)
The desert makes the desert: Climate feedbacks from the vegetation of arid zones
121(32)
Geography makes deserts
121(1)
But deserts make themselves
122(10)
The Sahel and vegetation feedbacks
127(5)
Have humans really caused the Sahelian droughts?
132(1)
Could the Sahara be made green?
132(4)
A human effect on climate? The grasslands of the Great Plains in the USA
136(3)
The Green Sahara of the past
139(4)
Could other arid regions show the same amplification of change by vegetation cover?
143(2)
Dust
145(5)
Sudden climate switches and dust
149(1)
The future
150(3)
Forests
153(28)
Finding out what forests really do to climate
155(6)
What deforestation does to climate within a region
161(8)
Re-afforestation
169(1)
The remote effects of deforestation
169(1)
The role of forest feedback in broad swings in climate
170(6)
Deforestation and the Little Ice Age
170(3)
Deforestation around the Mediterranean and drying in North Africa
173(1)
Forest feedbacks during the Quaternary
173(3)
Volatile organic compounds and climate
176(1)
Forest-climate feedbacks in the greenhouse world
177(4)
Plants and the carbon cycle
181(40)
The ocean
183(2)
Plants as a control on CO2 and O2
185(2)
Methane: the other carbon gas
187(11)
Carbon and the history of the earth's temperature
188(1)
Plants, weathering and CO2
189(4)
Plants, CO2 and ice ages
193(5)
Humans and the carbon store of plants
198(3)
The present increase in CO2
201(9)
The oceans as a carbon sink
204(1)
Seasonal and year-to-year wiggles in CO2 level
205(5)
The signal in the atmosphere
210(2)
The strength of the seasonal ``wiggle'' in CO2
212(1)
Accounting errors: the missing sink
213(2)
Watching forests take up carbon
215(6)
Predicting changes in global carbon balance under global warming
217(4)
The direct carbon dioxide effect on plants
221(40)
The two direct effects of CO2 on plants: photosynthesis and water balance
221(1)
Increased CO2 effects at the scale of a leaf
222(1)
Modeling direct CO2 effects
223(1)
What models predict for increasing CO2 and global vegetation
224(1)
Adding climate change to the CO2 fertilization effect
225(2)
Experiments with raised CO2 and whole plants
227(6)
The sort of results that are found in CO2 enrichment experiments
230(3)
A decline in response with time
233(1)
Temperature and CO2 responses interacting
233(1)
A few examples of what is found in FACE experiments
234(8)
Forests
234(2)
Semi-desert and dry grassland vegetation
236(1)
Will C4 plants lose out in an increased CO2 world?
237(5)
Other FACE experiments
242(2)
FACE studies on agricultural systems
242(2)
Some conclusions about FACE experiments
244(1)
Will a high CO2 world favor C3 species over C4 species?
244(1)
What factors tend to decrease plant responses to CO2 fertilization?
245(1)
There are other effects of enhanced CO2 on plants apart from growth rate
245(1)
CO2 fertilization and soils
246(1)
CO2 fertilization effects across trophic levels
247(6)
Looking for signs of a CO2 fertilization effect in agriculture
248(1)
Looking for signs of a CO2 fertilization effect in natural plant communities
249(3)
The changing seasonal amplitude of CO2
252(1)
CO2 levels and stomata out in nature
253(1)
Direct CO2 effects and the ecology of the past
253(5)
Direct CO2 effects on longer geological timescales
256(1)
Ancient moist climates or high CO2 effects?
257(1)
Other direct CO2 effects: in the oceans
258(1)
The future direct CO2 effect: a good or a bad thing for the natural world?
259(1)
Conclusion: The limits to what we can know
260(1)
Bibliography 261(4)
Index 265
Jonathan Adams has a very diverse background in the environmental sciences, including biogeography, classical ecology, Quaternary geology and earth system science. He has published in international journals on all of these topics and collaborated with some of the best known scientists in these fields. He has also organized meetings and edited special issues of journals on earth system science. Thus, he has the inter-disciplinary knowledge necessary to tackle a subject as far-reaching and many-faceted as vegetation-climate interactions, on a range of spatial scales and time scales.