Cosmologies and Regionalisms from "Above' and "Below' in the Post-Cold War Americas: the Relevance of Karl Polanyi for the 21st Century

Drawing on a Polanyian analysis of the land question, this article aims to analyse both Western and Indigenous cosmologies of Abya Yalathe name that indigenous peoples give to the American continentto understand the relationship between human beings and land and nature. These cosmologies are at the heart of the way in which two distinct societies construct their regional space, one from above', the other from below', and they are therefore key to understanding today's climate change problematique. Following this nexus it is argued that, since the end of the Cold War, a new regional double-movement', unleashed by the quest for land and natural resources has been in the making. This is a superstructural or legal battle between Western transnational regime-making and a law that originated at the centre of the Earth'. The article explains both regionalisms and the dialectical interaction between them and demonstrates that Karl Polanyi's legacy remains relevant for the 21st century.

Use of Land Surface Temperature to Estimate Surface Energy Fluxes: Contributions of Wilfried Brutsaert and Collaborators

Land surface temperature (LST) plays a key role in governing the land surface energy budget, and measurements or estimates of LST are an integral part of many land surface models and methods to estimate land surface sensible heat (H) and latent heat fluxes. In particular, the LST anchors the potential temperature profile in Monin-Obukhov similarity theory, from which H can be derived. Brutsaert has made important contributions to our understanding the nature of surface temperature measurements as well as the practical but theoretically sound use of LST in this framework. His work has coincided with the wide-spread availability of remotely sensed LST measurements. Use of remotely sensed LST estimates inevitably involves complicating factors, such as: varying spatial and temporal scales in measurements, theory, and models; spatial variability of LST and H; the relationship between measurements of LST and the temperature felt by the atmosphere; and the need to correct satellite-based radiometric LST measurements for the radiative effects of the atmosphere. This paper reviews the progress made in research in these areas by tracing and commenting on Brutsaert's contributions.