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Ocean Salinities Reveal Strong Global Water Cycle Intensification During 1950 to 2000
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Fundamental thermodynamics and climate models suggest that dry regions will become drier
and wet regions will become wetter in response to warming. Efforts to detect this long-term
response in sparse surface observations of rainfall and evaporation remain ambiguous. We show
that ocean salinity patterns express an identifiable fingerprint of an intensifying water cycle.
Our 50-year observed global surface salinity changes, combined with changes from global climate
models, present robust evidence of an intensified global water cycle at a rate of 8 T 5% per degree
of surface warming. This rate is double the response projected by current-generation climate
models and suggests that a substantial (16 to 24%) intensification of the global water cycle will
occur in a future 2° to 3° warmer world.
SCIENCE VOL 336
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OCEAN–ATMOSPHERE COUPLING Mesoscale eddy effects
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1st paragraph: Because of its enormous heat capacity, the ocean plays a critical role in regulating the Earth’s climate. Up to about a decade ago, it was generally believed that, outside the tropics, the ocean responds only passively to atmospheric forcing1. However, with the advent of satellite measurements of sea surface temperature and surface winds with resolutions down to about 50 km, it became apparent that the strong gradients in sea surface temperature that are associated with meanders in the Gulf Stream, the California Current and most other ocean currents can directly affect surface winds1–3.
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Ohio Department of Natural Resources: Division of Forestry
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The Division of Forestry is responsible for the management, sustainable use, and protection of Ohio’s forests.
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Oklahoma 1997.pdf
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OLD National Capital Region's Biennial Spotlight on National Park Resources
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Old Trees: Extraction, Conservation Can Coexist
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BECAUSE LARGE OLD TREES ARE ESSENTIAL FOR FOREST ECOSYSTEM INTEGRITY AND BIODIVERsity,
timber extraction in managed forests should preferentially be concentrated where large old
trees are least likely to develop (“Global decline in large old trees,” D. B. Lindenmayer et al.,
Perspectives, 7 December 2012, p. 1305). However, timber extraction and the conservation of
large old trees are not necessarily mutually exclusive.
Current forest policy and management practices in Flanders, Belgium, aim to convert
even-aged stands (areas in which trees are all the same age) to stands with trees of varying
ages in an effort to increase forest ecosystem stability and resilience and to allow trees to
grow old. As part of their ecologically sustainable forest management, public forest managers
have adopted a large-tree retention approach [see also (1, 2)]. Tree islands within
stands managed for production of high-quality timber are reserved for conservation, and
trees within these islands will never be extracted. Large old trees of commercially valuable
species that have grown beyond the commercially optimal dimensions will
not be logged either. And no tree beyond a threshold diameter [currently set at
dbh (diameter at breast height) of more than 102 cm] will ever be logged. The
strip-shelterwood system (in which trees are cut in linear strips and surrounding
trees are given time to grow old) and the coppice-with-standards system
(in which some trees are left to grow while others around them are cut) are
two examples of forest management that allows the combination of sustainable
forest exploitation and conservation of large old trees
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Old Tutorial
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RPCCR Tutorial
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Old-growth forests as global carbon sinks
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Old-growth forests remove carbon dioxide from the atmosphere1,2 at rates that vary with climate and nitrogen deposition3. The seques- tered carbon dioxide is stored in live woody tissues and slowly decomposing organic matter in litter and soil4. Old-growth forests therefore serve as a global carbon dioxide sink, but they are not protected by international treaties, because it is generally thought that ageing forests cease to accumulate carbon5,6. Here we report a search of literature and databases for forest carbon-flux estimates. We find that in forests between 15 and 800 years of age, net ecosys- tem productivity (the net carbon balance of the forest including soils) is usually positive. Our results demonstrate that old-growth forests can continue to accumulate carbon, contrary to the long- standing view that they are carbon neutral. Over 30 per cent of the global forest area is unmanaged primary forest, and this area con- tains the remaining old-growth forests7. Half of the primary forests (6 3 108 hectares) are located in the boreal and temperate regions of the Northern Hemisphere. On the basis of our analysis, these forests alone sequester about 1.3 6 0.5 gigatonnes of carbon per year. Thus, our findings suggest that 15 per cent of the global forest area, which is currently not considered when offsetting increasing atmospheric carbon dioxide concentrations, provides at least 10 per cent of the global net ecosystem productivity8. Old-growth forests accumulate carbon for centuries and contain large quantities of it. We expect, however, that much of this carbon, even soil carbon9, will move back to the atmosphere if these forests are disturbed.
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Old-Growth Forests Can Accumulate Carbon in Soils
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1st paragraph: ld-growth forests have traditionally been considered negligible as carbon sinks because carbon uptake has been thought to be balanced by respiration (1). We show that soils in the top 20-cm soil layer in preserved old-growth forests in southern China accumulated atmospheric carbon at an unexpectedly high rate from 1979 to 2003. This phenomenon indicates the need for future research on the complex responses and adaptation of belowground processes to global environmental change.
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Oligocene CO2 Decline Promoted C4 Photosynthesis in Grasses
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C4 photosynthesis is an adaptation derived from the more common C3 photosynthetic pathway that con- fers a higher productivity under warm temperature and low atmospheric CO2 concentration [1, 2]. C4 evolution has been seen as a consequence of past atmospheric CO2 decline, such as the abrupt CO2 fall 32–25 million years ago (Mya) [3–6]. This relationship has never been tested rigorously, mainly because of a lack of accurate estimates of divergence times for the different C4 lineages [3]. In this study, we inferred a large phylogenetic tree for the grass family and es- timated, through Bayesian molecular dating, the ages of the 17 to 18 independent grass C4 lineages. The first transition from C3 to C4 photosynthesis occurred in the Chloridoideae subfamily, 32.0–25.0 Mya. The link between CO2 decrease and transition to C4 pho- tosynthesis was tested by a novel maximum likeli- hood approach. We showed that the model incorpo- rating the atmospheric CO2 levels was significantly better than the null model, supporting the importance of CO2 decline on C4 photosynthesis evolvability. This finding is relevant for understanding the origin of C4 photosynthesis in grasses, which is one of the most successful ecological and evolutionary innovations in plant history.
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