We used the handbook as developed by Frans Geilfus, which covers 80 tools for participatory development as an important base for this tools guide. A selection. Geilfus, Frans. 80 tools for participatory development: appraisal, planning, follow- up and evaluation / Frans Geilfus. — San Jose, C.R.: IICA,. p. ; 24 cm. Title: “80 Herramientas para el desarrollo participativo” de Frans Geilfus (IICA, ), Author: brenda chau pasco, Name: “80 Herramientas para el desarrollo.
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One of the relevant aspects that peasants consider is the corncob health, which is of vital importance to obtain better germination of the seed. Large tundra methane burst during onset of freezing.
Clearly, enhanced focus on responses towards reduced sea ice cover and enhanced run-off in the coastal Arctic is required to assess the changes in net productivity given projected climate change in the region.
Ali, Genevieve, Claire J. Methane production in aerobic oligotrophic surface water in the central Arctic Ocean. Arctic Ocean surface warming trends fans the past years. A significant increase was shown for November—December, however, which was attributed to increases in late-season emissions.
Journal of Phycology49, — He is an oceanographer and climate researcher interested in circulation and biogeochemical cycles in the ocean. Geochemical and geophysical evidence of methane release over the East Siberian Arctic Shelf.
To grasp the breadth of consequences following from permafrost thaw, ESMs need to better represent thermokarst processes and the flows of carbon between the land and the ocean. Moreover, the dissimilar warming from sea ice decline throughout the year may lead to varying responses in respiration, photosynthesis, and methane frand that currently may be underappreciated.
He must decide whether to use or not some agrichemicals fertilizers, insecticides, herbicides, etc.
On the other hand, the regions that practice entrepreneurial agriculture lean on their use of pesticides, fertilizers, machinery, improved seed, etc. Dependent on relative responses of photosynthesis and respiration.
Large uncertainties remain, however, on the ffrans development of the various components of the arctic carbon cycle, under pressure from permafrost thaw and sea ice decline.
A winter flux time series.
80 herramientas para el desarrollo participativo: diagnóstico, planificación …
Sensitivity of the carbon cycle in the Arctic to climate change. This could potentially lead to reduced primary production in surface waters. On the other hand, dissolved OC concentrations are significantly higher in permafrost-free versus permafrost-dominated sub-watersheds in west Siberian peatlands Frey et al.
Extensive release of methane from Arctic seabed west of Svalbard during summer does not influence the atmosphere. These estimates are in line with Jutterstrom and Andersonwho predicted an increase in uptake of 1.
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Increased emission, but compensated by photosynthesis. Changes and trends in lateral carbon flows Changes in the arctic hydrological cycle, e. This would allow through time to develop a maize type or variety that adjusts to their preferences in an integral manner. Marine carbon cycling Carbon exchange between water and atmosphere Changes in arctic sea ice cover, the marine ecosystem, and the hydrological cycle could significantly affect the amount of CO 2 that is absorbed from the atmosphere by the Arctic Ocean typically defined as the ocean waters North of the Arctic circle.
Adapted from Miller et al. Uptake of CO 2 by the Arctic Ocean in a changing climate. The identification performed by peasants of the size of the corncob as main characteristic is in relation to the conditions of rainfed agriculture that is practiced, which requires sowing at a greater depth and, therefore, requires seed with higher reserve content to emerge. Current estimates of franz rates through ice suggest that this exchange may be insignificant compared to direct air—sea exchange Loose et al.
The population is the peasant families heads of households. Implications for mixed-layer ventilation of CO2 in the seasonal ice zone. A parameter model of gfilfus exchange for the seasonal sea ice zone. Permafrost thaw, and tundra fires, can act as a positive feedback. Articles Traditional selection of creole maize seed.
To the northwest there are schools, the church, the health center, and the market. Riverine-driven interhemispheric transport of carbon.
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Annual Review of Marine Science. A circumpolar perspective on fluvial sediment flux to the Arctic ocean. The presence or absence of water, snow, and ice plays an important role in determining the rate of carbon release from thawing permafrost as well as its eventual release into the atmosphere.
An assessment of the carbon balance of Arctic tundra: Benthic microalgal production in the Arctic: Airborne measurements also inherently include previously often neglected sources such as freshwater systems and geologic sources, which can be significant sources of methane and CO 2 Walter Anthony et al. Arctic marginal ice zone trending wider in summer and narrower in winter.
Methane emissions from permafrost thaw lakes limited by lake drainage. CH 4 production ratio lowest for tundra sitesand in overall anaerobic CO 2 and methane production greatest for organic soils and inundated soils, and least for deeper horizons.
Model studies of the Arctic Ocean have resulted in an uptake of 0. Soil carbon in the Arctic and the permafrost carbon feedback. The selection pressure on one characteristic can be an indicator of how the selection carried out by the peasant generates diversity in maize varieties in one region. Indeed, an analysis of an year dataset of carbon exchange in Zackenberg showed that higher temperatures did not stimulate photosynthesis in the long term, while still raising respiration Lund et al.
Most of the peasants in the region carry out the seed selection when the corncob is already formed, choosing that of greatest uniformity, greater size, and free of pests and diseases.
For example, an analysis of three decades of atmospheric measurements in Barrow, Alaska, showed that methane emissions had not increased despite increasing temperatures in the region Sweeney et al. His research interests fras the surface-atmosphere exchange of carbon dioxide and methane in degraded peatlands and Geilgus permafrost environments. Seasonal carbon cycling in a Greenlandic fjord: Introduction From the perspective of an astronaut, looking down on the Earth high above the North Pole, it is self-evident that the marine and terrestrial carbon cycles of the Arctic cannot be considered separately.