498 research outputs found
Interpreting forest diversity-productivity relationships : volume values, disturbance histories and alternative inferences
Understanding the relationship between stand-level tree diversity and productivity has the potential to inform the science and management of forests. History shows that plant diversity-productivity relationships are challenging to interpret—and this remains true for the study of forests using non-experimental field data. Here we highlight pitfalls regarding the analyses and interpretation of such studies. We examine three themes: 1) the nature and measurement of ecological productivity and related values; 2) the role of stand history and disturbance in explaining forest characteristics; and 3) the interpretation of any relationship. We show that volume production and true productivity are distinct, and neither is a demonstrated proxy for economic values. Many stand characteristics, including diversity, volume growth and productivity, vary intrinsically with succession and stand history. We should be characterising these relationships rather than ignoring or eliminating them. Failure to do so may lead to misleading conclusions. To illustrate, we examine the study which prompted our concerns —Liang et al. (Science 354:aaf8957, 2016)— which developed a sophisticated global analysis to infer a worldwide positive effect of biodiversity (tree species richness) on “forest productivity” (stand level wood volume production). Existing data should be able to address many of our concerns. Critical evaluations will improve understanding.</p
More trees for more water in drylands: myths and opportunities
The mechanisms by which trees influence water availability remain incompletely understood, but the last two decades have brought astonishing advances. We already know enough to see major opportunities to improve water security in tropical drylands through tree cover, while also yielding the many other benefits that trees provide
Wood decomposition is more rapid on than off termite mounds in an African savanna
Decomposition is important for nutrient cycling and the dynamics of soil organic matter. The factors that influence local decomposition rates in savannas dominated by Macrotermes mounds remain uncertain. Here, we experimentally assessed the effects of macro- and micro-detritivores, active and inactive mounds, and vegetation cover on wood decomposition rates for eight common woody plant species in Lake Mburo National Park, in Uganda. Five pairs of Macrotermes mounds, one active and one inactive per pair, were selected. Each mound provided two sample locations, one, the most shaded (with canopy cover), and one, the most open (without canopy cover) edge of mound. In addition, for each mound pair, one additional sample location was
located off-mound, in an open level area between the mounds. After one, three, and 12 months, protected (wrapped in 1-mm mesh fiber-glass excluding macrodetritivores) and unprotected wood samples from each location were retrieved, brushed clean, oven-dried, and weighed. After 12 months, mean percentage mass loss was four times higher for unprotected than protected wood samples across all species located on mound sites
(when decomposition in shaded and open microhabitats was combined). Mean percentage mass loss across all species combined was 1.2 times higher on active than inactive mounds. Across all mounds, decomposition was on average 1.1 times more rapid in the shaded than open mound parts. These differences were more pronounced on inactive mounds (1.3 times more rapid in the shaded than open parts). Percentage mass loss was markedly lower off-mound (12.6 0.8%) than on active (25.9 1.5%) or inactive mounds (19.7 1.2%). Proportional mass loss for unprotected wood decreased with increasing wood density, but proportional mass loss of protected wood samples was not detectably influenced by wood density. Our study highlights the strong and locally contingent influence of termite mounds, termite activity, vegetation, and their interactions on wood decomposition rates within a savanna landscape. Furthermore, variation in per-species wood decomposition rates, including the negative correlation with wood density, depends on accessibility to macrodetritivores.publishedVersio
The water budget of a hurricane as dependent on its movement
Despite the dangers associated with tropical cyclones and their rainfall, the
origins of storm moisture remains unclear. Existing studies have focused on the
region 40-400 km from the cyclone center. It is known that the rainfall within
this area cannot be explained by local processes alone but requires imported
moisture. Nonetheless, the dynamics of this imported moisture appears unknown.
Here, considering a region up to three thousand kilometers from storm center,
we analyze precipitation, atmospheric moisture and movement velocities for
North Atlantic hurricanes. Our findings indicate that even over such large
areas a hurricane's rainfall cannot be accounted for by concurrent evaporation.
We propose instead that a hurricane consumes pre-existing atmospheric water
vapor as it moves. The propagation velocity of the cyclone, i.e. the difference
between its movement velocity and the mean velocity of the surrounding air
(steering flow), determines the water vapor budget. Water vapor available to
the hurricane through its movement makes the hurricane self-sufficient at about
700 km from the hurricane center obviating the need to concentrate moisture
from greater distances. Such hurricanes leave a dry wake, whereby rainfall is
suppressed by up to 40 per cent compared to its long-term mean. The inner
radius of this dry footprint approximately coincides with the radius of
hurricane self-sufficiency with respect to water vapor. We discuss how Carnot
efficiency considerations do not constrain the power of such open systems that
deplete the pre-existing moisture. Our findings emphasize the incompletely
understood role and importance of atmospheric moisture supplies, condensation
and precipitation in hurricane dynamics.Comment: 38 pages, 17 figures, 1 Table; extended analyses: available E/P
ratios reviewed and explained (Table 1); rainfall and moisture distributions
3 days before and after hurricanes, propagation velocity and its relationship
to radial velocity; efficiency for non-steady hurricanes; hurricane motion
and rainfall asymmetries discusse
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