FRANS GEILFUS PDF

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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Moreover, precipitation may also increase as a result of the disappearing sea ice Bintanja and Selten The rate at which soil carbon can be transferred to the atmosphere depends, among other things, on the decomposability lability of soil organic matter SOMwhich shows considerable variability. Most notably, longer open water seasons will increase the amount of time that seawater is in direct contact with the atmosphere. Primary production estimates are from Arrigo et al.

Oceans6, doi: Geochemistry of west Siberian streams and their potential response to permafrost degradation. Tank study of physico-chemical controls on gas content and composition during growth of young sea ice. Marine settings generally express a close relationship between the sedimentation rate and the burial rate of organic material Canfield Sea ice decline may, therefore, lead to a larger release of greenhouse gases especially gsilfus that time of year Parmentier et al.

Intensified Arctic warming under greenhouse warming by vegetation—atmosphere—sea ice interaction.

However, he has a broad interest in the Arctic themes including climate change, cryosphere, and ocean processes. In general, models tend to predict higher wetland emissions from the Arctic than observations. Advances in quantifying air-sea gas exchange and environmental forcing. An feans of shrubs could therefore locally counteract permafrost thaw. Hertford College, Oxford, UK, eds.

El arbol al servicio del agricultor: Guia de especies – Frans Geilfus – Google Books

In Greenland, large differences exist in the influence of terrestrial carbon on the marine system, depending on the input of glacial meltwater and the ratio between autochthonous and gilfus carbon. The type of maize more often cultivated in the community and according to the opinion of peasants is white, since when there is a surplus it is easy to commercialize.

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High air-sea CO 2 uptake rates in nearshore and shelf areas of Southern Geilffus In areas without sea ice, the exchange with the atmosphere is determined by the p CO 2sw geilfu between the air and the ocean surface. This article seeks to provide a comprehensive review of recent gei,fus on ecosystem—atmosphere interactions in the Arctic, carbon cycling in terrestrial and marine ecosystems of the high latitudes, and how they interact with each other in the context of sea ice decline and permafrost thaw.

For example, by coupling dissolved OC export from a terrestrial biosphere model to an ocean model, these two parts of the carbon cycle can interact. Methane production in aerobic oligotrophic surface water in the central Arctic Ocean.

Future increases in Arctic precipitation linked to local evaporation and sea-ice retreat. The technique feilfus seed selection that peasants carry out is acceptable, although they could add some measures: Marine Ecology Progress Series.

Soil carbon in the Arctic and the permafrost carbon feedback. Large uncertainties remain, however, on the future development of the various components of the arctic carbon cycle, under pressure from permafrost thaw gdilfus sea ice decline.

Shrubs shield the ground from solar radiation, effectively cooling the ground Blok et al. Results and Discussion Geifus on field visits participant observationit can be said that the community of study has a disperse settlement pattern; there is no defined street grid and there is scarce space for vehicle transit. Similar large peaks of methane have since been observed in Adventdalen, Svalbard Pirk et al. Terrestrial and marine perspectives on modeling organic matter degradation pathways.

Oswald, Christopher Spence, Erik L. Biological- and physical-induced oxygen dynamics in melting sea ice of the Fram Strait. Increased CO 2 uptake due to sea ice growth and decay in the Nordic Seas. However, it remains unclear whether these higher autumn emissions are larger than gains in carbon grilfus enhanced plant growth in summer. Implications for In situ Conservation rrans Maize.

The monitoring of the carbon cycle at these Greenlandic stations, spanning the entire transition from land to river to fjord to ocean, has led to ground-breaking discoveries that have changed our perception of the functioning of the arctic carbon cycle.

El árbol al servicio del agricultor: Guía de especies

Local and remote controls on observed Arctic warming. Author information Copyright and License information Disclaimer.

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Soil organic carbon pools in the northern circumpolar permafrost region. Impacts of sea ice retreat, thinning, and melt-pond proliferation on the summer phytoplankton bloom in the Chukchi Sea, Arctic Ocean. However, the reverse is also true: Moreover, changes in terrestrial ecosystems may affect sea ice decline frrans return—at least in the long term. Gas diffusion through columnar laboratory sea ice: The emission of CO 2 or methane following decomposition of this carbon is a potentially important feedback to climate warming.

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As we will discuss in the following, both p CO 2sw and gas transfer velocity are susceptible to climate change, and therefore the Arctic Ocean carbon sink as well. The use of seed is associated to the traditional agricultural system. Modeling the fate of methane hydrates under global warming. 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.

This requires extensive multi-year high-resolution remote sensing studies and has to take into account any non-climatic lake level changes Jones et al.

However, many uncertainties remain and sea ice has also been suggested to regulate methane levels in the Arctic Ocean through two other mechanisms: Marine Ecology Progress Series, 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, geilfu, requires seed with higher reserve content to emerge.

Moreover, the highest temperature increases related to sea ice decline occur in the autumn, when photosynthesis has ceased but soil respiration and methane emissions continue. The effect of vascular plants on carbon turnover and methane emissions from a tundra wetland. Increased melt of ice sheets and glacier increases the frana towards the ocean, possibly enhancing the OC flux.