Minding the Mental: Intentionality, Consciousness, and Daniel Dennett in Contemporary Philosophy of Mind

The mind. Sanctum sanctorum of subjectivity. Soundstage of the mental. Consciousness\u27 cockpit. Romping-grounds of the intentional. A great deal, it would seem, rides on the notion of mind. It\u27s not just that naughty children never do, or that people when irritated often claim to have half-a-one. Though perhaps telling in other ways, it isn\u27t so important that while we all think we lose ours from time to time, we rarely-if ever-doubt that we had one to begin with. Solipsists are perfectly willing to doubt that anyone else actually possesses one, but no one suspects that everyone but herself has one. The reason seems clear and distinct as Cartesian water; it just makes sense, which is another thing that minds are rumored to be responsible for. One could go on and on-the idioms seem endless-but nevermind

Global maps of soil temperature

Research in global change ecology relies heavily on global climatic grids derived from estimates of air temperature in open areas at around 2 m above the ground. These climatic grids do not reflect conditions below vegetation canopies and near the ground surface, where critical ecosystem functions occur and most terrestrial species reside. Here, we provide global maps of soil temperature and bioclimatic variables at a 1-km² resolution for 0–5 and 5–15 cm soil depth. These maps were created by calculating the difference (i.e., offset) between in-situ soil temperature measurements, based on time series from over 1200 1-km² pixels (summarized from 8500 unique temperature sensors) across all the world’s major terrestrial biomes, and coarse-grained air temperature estimates from ERA5-Land (an atmospheric reanalysis by the European Centre for Medium-Range Weather Forecasts). We show that mean annual soil temperature differs markedly from the corresponding gridded air temperature, by up to 10°C (mean = 3.0 ± 2.1°C), with substantial variation across biomes and seasons. Over the year, soils in cold and/or dry biomes are substantially warmer (+3.6 ± 2.3°C) than gridded air temperature, whereas soils in warm and humid environments are on average slightly cooler (-0.7 ± 2.3°C). The observed substantial and biome-specific offsets emphasize that the projected impacts of climate and climate change on near-surface biodiversity and ecosystem functioning are inaccurately assessed when air rather than soil temperature is used, especially in cold environments. The global soil-related bioclimatic variables provided here are an important step forward for any application in ecology and related disciplines. Nevertheless, we highlight the need to fill remaining geographic gaps by collecting more in-situ measurements of microclimate conditions to further enhance the spatiotemporal resolution of global soil temperature products for ecological applications

Proceedings of the 13th annual conference of INEBRIA

CITATION: Watson, R., et al. 2016. Proceedings of the 13th annual conference of INEBRIA. Addiction Science & Clinical Practice, 11:13, doi:10.1186/s13722-016-0062-9.The original publication is available at https://ascpjournal.biomedcentral.comENGLISH SUMMARY : Meeting abstracts.https://ascpjournal.biomedcentral.com/articles/10.1186/s13722-016-0062-9Publisher's versio

Global maps of soil temperature.

Research in global change ecology relies heavily on global climatic grids derived from estimates of air temperature in open areas at around 2 m above the ground. These climatic grids do not reflect conditions below vegetation canopies and near the ground surface, where critical ecosystem functions occur and most terrestrial species reside. Here, we provide global maps of soil temperature and bioclimatic variables at a 1-km2 resolution for 0-5 and 5-15 cm soil depth. These maps were created by calculating the difference (i.e. offset) between in situ soil temperature measurements, based on time series from over 1200 1-km2 pixels (summarized from 8519 unique temperature sensors) across all the world's major terrestrial biomes, and coarse-grained air temperature estimates from ERA5-Land (an atmospheric reanalysis by the European Centre for Medium-Range Weather Forecasts). We show that mean annual soil temperature differs markedly from the corresponding gridded air temperature, by up to 10°C (mean = 3.0 ± 2.1°C), with substantial variation across biomes and seasons. Over the year, soils in cold and/or dry biomes are substantially warmer (+3.6 ± 2.3°C) than gridded air temperature, whereas soils in warm and humid environments are on average slightly cooler (-0.7 ± 2.3°C). The observed substantial and biome-specific offsets emphasize that the projected impacts of climate and climate change on near-surface biodiversity and ecosystem functioning are inaccurately assessed when air rather than soil temperature is used, especially in cold environments. The global soil-related bioclimatic variables provided here are an important step forward for any application in ecology and related disciplines. Nevertheless, we highlight the need to fill remaining geographic gaps by collecting more in situ measurements of microclimate conditions to further enhance the spatiotemporal resolution of global soil temperature products for ecological applications

A Randomized Trial of Three Psychosocial Treatments for the Symptoms of Rheumatoid Arthritis

OBJECTIVE: To assess and compare the benefits of three psychosocial treatments for rheumatoid arthritis. METHODS: Rheumatoid arthritis (RA) patients were randomized to cognitive-behavior therapy (CBT), relaxation response training (RR), or arthritis education (AE). All treatment was conducted in groups. Follow-up occurred immediately after treatment and 6 and 12 months later. Pain, other RA symptoms, role impairment, and psychological distress were assessed with standardized self-report questionnaires. Arthritis severity and activity were assessed with a joint examination, erythrocyte sedimentation rate, grip strength, and walking time. An intent-to-treat analytic strategy was employed. Linear regression was used to establish treatment effect on pain and other RA symptoms, while adjusting for sociodemographic and clinical variables. RESULTS: 168 patients were randomized. Pain improved significantly at 12 months in the RR and AE groups and showed a non-significant positive trend with CBT. Other RA symptoms improved significantly with CBT and AE, and showed a non-significant trend with RR. There were no significant differences in the outcomes across the 3 treatment groups. When the results for all 3 groups were aggregated, significant benefits were found for pain, other RA symptoms, self-care activities and social activities. Effect sizes ranged between 0.26 and 0.35. CONCLUSIONS: These three psychosocial treatments were beneficial, with treatment effect sizes in the small to moderate range. The effects appeared immediately after treatment and were generally sustained at long-term follow-up. These benefits were achieved over and above those resulting from medical management. These treatments constitute an effective augmentation to standard medical therapy for rheumatoid arthritis patients