Informal Recycling Sector (IRS), Contribution to the Achievement of the SDGs, and a Circular Economy

status: Published onlin

[Policy Brief] Decarbonization is not green: overcoming the unspoken issues of a low-carbon world

The decarbonization policies of Northern economies are unsustainably increasing demand for “critical energy transition minerals”, whose deposits are mainly located in Southern countries. Improving recycling capacities will not be enough to meet these growing needs. Only equitable sufficiency policies, relocation and responsible management of mining activities are likely to make the mining future more sustainable and equitable

[Policy Brief] Decarbonization is not green: overcoming the unspoken issues of a low-carbon world

The decarbonization policies of Northern economies are unsustainably increasing demand for “critical energy transition minerals”, whose deposits are mainly located in Southern countries. Improving recycling capacities will not be enough to meet these growing needs. Only equitable sufficiency policies, relocation and responsible management of mining activities are likely to make the mining future more sustainable and equitable

[Policy Brief] Decarbonization is not green: overcoming the unspoken issues of a low-carbon world

The decarbonization policies of Northern economies are unsustainably increasing demand for “critical energy transition minerals”, whose deposits are mainly located in Southern countries. Improving recycling capacities will not be enough to meet these growing needs. Only equitable sufficiency policies, relocation and responsible management of mining activities are likely to make the mining future more sustainable and equitable

High-resolution palaeoclimatology of the last millennium: A review of current status and future prospects

This review of late-Holocene palaeoclimatology represents the results from a PAGES/CLIVAR Intersection Panel meeting that took place in June 2006. The review is in three parts: the principal high-resolution proxy disciplines (trees, corals, ice cores and documentary evidence), emphasizing current issues in their use for climate reconstruction; the various approaches that have been adopted to combine multiple climate proxy records to provide estimates of past annual-to-decadal timescale Northern Hemisphere surface temperatures and other climate variables, such as large-scale circulation indices; and the forcing histories used in climate model simulations of the past millennium. We discuss the need to develop a framework through which current and new approaches to interpreting these proxy data may be rigorously assessed using pseudo-proxies derived from climate model runs, where the 'answer' is known. The article concludes with a list of recommendations. First, more raw proxy data are required from the diverse disciplines and from more locations, as well as replication, for all proxy sources, of the basic raw measurements to improve absolute dating, and to better distinguish the proxy climate signal from noise. Second, more effort is required to improve the understanding of what individual proxies respond to, supported by more site measurements and process studies. These activities should also be mindful of the correlation structure of instrumental data, indicating which adjacent proxy records ought to be in agreement and which not. Third, large-scale climate reconstructions should be attempted using a wide variety of techniques, emphasizing those for which quantified errors can be estimated at specified timescales. Fourth, a greater use of climate model simulations is needed to guide the choice of reconstruction techniques (the pseudo-proxy concept) and possibly help determine where, given limited resources, future sampling should be concentrated

Temporal Growth Variation in High-Elevation Forests: Case Study of Polylepis Forests in Central Andes

Polylepis species form the dominant high-altitude forests in the tropicalAndes, one of the most vulnerable regions to future climate change scenarios. Thestudy of the growth of these forests provides useful information about their ontogenyand the environmental conditions where they develop. The identification ofgrowth patterns is relevant for understanding the dynamics of the forests in responseto climatic variables. In this chapter, we present a brief review of dendroecologicalstudies on Polylepis species. We also developed for the first time in the centralAndes of Peru three new Polylepis ring-width chronologies together with a diametergrowth modeling for the following species: Polylepis rodolfo-vasquezii, Polylepisrugulosa, and Polylepis tarapacana. Dendrochronological techniques together with a biologically based model help us to obtain information on forestry traits ofPolylepis species. P. rodolfo-vasquezii to growth response to summer temperature ofthe current growth period determined radial growth, whereas spring and summerprecipitation from the previous growth period determined the radial growth in P.rugulosa and P. tarapacana, respectively. The radial growth models indicated differencesin the growth of the three Polylepis species with P. rodolfo-vasquezii reachingthe highest rate (0.11 cm/yr), while P. tarapacana showed the lowest (0.08 cm/yr). Due to the low growth rates of these Polylepis species, long periods (>100 years)are required to establish and provide ecosystem services. As these forests face thechallenge of climate change and anthropogenic pressure, there is a clear need toobtain precise information in order to formulate guidelines for the conservation ofthese forests, and the application of dendroecology is indispensable in this context.Fil: Requena Rojas, Edilson Jimmy. Universidad Continental; PerúFil: Crispín DelaCruz, Doris B.. Universidad Continental; PerúFil: Ticse-Otarola, Ginette. Universidad Continental; PerúFil: Rusbelth Quispe Melgar, Harold. Universidad Continental; PerúFil: Inga Guillen, Janet G.. Universidad Continental; PerúFil: Camel Paucar, Vladimir. Universidad Nacional Agraria La Molina; PerúFil: Guerra, Anthony. Universidad Nacional del Centro del Perú; PerúFil: Ames Martinez, Fressia Nathalie. Universidad Continental; PerúFil: Morales, Mariano Santos. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentin