Introduction

Husserl’s philosophy, by the usual account, evolved through three stages: 1. development of an anti-psychologistic, objective foundation of logic and mathematics, rooted in Brentanian descriptive psychology; 2. development of a new discipline of "phenomenology" founded on a metaphysical position dubbed "transcendental idealism"; transformation of phenomenology from a form of methodological solipsism into a phenomenology of intersubjectivity and ultimately (in his Crisis of 1936) into an ontology of the life-world, embracing the social worlds of culture and history. We show that this story of three revolutions can provide at best a preliminary orientation, and that Husserl was constantly expanding and revising his philosophical system, integrating views in phenomenology, ontology, epistemology and logic with views on the nature and tasks of philosophy and science as well as on the nature of culture and the world in ways that reveal more common elements than violent shifts of direction. We argue further that Husserl is a seminal figure in the evolution from traditional philosophy to the characteristic philosophical concerns of the late twentieth century: concerns with representation and intentionality and with problems at the borderlines of the philosophy of mind, ontology, and cognitive science

Global analysis of night marine air temperature and its uncertainty since 1880: the HadNMAT2 Dataset

An updated version of the Met Office Hadley Centre’s monthly night marine air temperature dataset is presented. It is available on a 5? latitude-longitude grid from 1880 as anomalies relative to 1961-1990 calendar-monthly climatological average night marine air temperature (NMAT). Adjustments are made for changes in observation height; these depend on estimates of the stability of the near surface atmospheric boundary layer. In previous versions of the dataset, ad hoc adjustments were also made for three periods and regions where poor observational practice was prevalent. These adjustments are re-examined. Estimates of uncertainty are calculated for every grid box and result from: measurement errors; uncertainty in adjustments applied to the observations; uncertainty in the measurement height and under-sampling. The new dataset is a clear improvement over previous versions in terms of coverage because of the recent digitization of historical observations from ships' logbooks. However, the periods prior to about 1890 and around World War 2 remain particularly uncertain and sampling is still sparse in some regions in other periods. A further improvement is the availability of uncertainty estimates for every grid box and every month. Previous versions required adjustments that were dependent on contemporary measurements of sea surface temperature (SST); to avoid these, the new dataset starts in 1880 rather than 1856. Overall agreement with variations of SST is better for the updated dataset than for previous versions, maintaining existing estimates of global warming and increasing confidence in the global record of temperature variability and change

Photoelectron diffraction: from phenomenological demonstration to practical tool

The potential of photoelectron diffraction—exploiting the coherent interference of directly-emitted and elastically scattered components of the photoelectron wavefield emitted from a core level of a surface atom to obtain structural information—was first appreciated in the 1970s. The first demonstrations of the effect were published towards the end of that decade, but the method has now entered the mainstream armoury of surface structure determination. This short review has two objectives: First, to outline the way that the idea emerged and the way this evolved in my own collaboration with Neville Smith and his colleagues at Bell Labs in the early years: Second, to provide some insight into the current state-of-the art in application of (scanned-energy mode) photoelectron diffraction to address two key issue in quantitative surface structure determination, namely, complexity and precision. In this regard a particularly powerful aspect of photoelectron diffraction is its elemental and chemical-state specificity

IHS Workshop: "Honest, Clean, Industrious”: Working Class Respectability

Histor

The Several Factors of (Self-)Consciousness

Abstract: In prior essays I have sketched a “modal model” of (self-) consciousness. That model “factors” out several distinct forms of awareness in the phenomenological structure of a typical act of consciousness. Here we consider implications of the model à propos of contemporary theories of consciousness (e.g. higher-order and self-representational forms of awareness). In particular, we distinguish phenomenality from other features of awareness in a conscious experience: “what it is like” to have an experience involves several different factors. Further, we should see these factors as typical of consciousness, rather than essential features, allowing that some elements of awareness may be absent while others are present in certain less typical cases.Keywords: (Self-)consciousness; Higher-order Theories of Consciousness; Self-representational Theories of Consciousness; Phenomenality; Phenomenological Theories of ConsciousnessI diversi elementi della (auto-)coscienzaRiassunto: In lavori precedenti ho cercato di proporre un “modello modale” della (auto)coscienza. Questo modello “considera” forme differenti e distinte di consapevolezza che sono presenti nella struttura fenomenologica di un atto tipico di coscienza. Qui intendo considerare alcune implicazioni di questo modello in relazione ad alcune teorie contemporanee della coscienza (tra cui, le teorie di alto livello della coscienza e le forme auto-rappresentazionali di consapevolezza). In particolare, distingueremo la fenomenicità da altre proprietà della consapevolezza all’interno di un’esperienza cosciente: il “che cosa si prova” a essere titolari un’esperienza implica elementi differenti e distinti. Inoltre, dovremo considerare questi elementi come caratteri tipici della coscienza e non come proprietà essenziali, riconoscendo che alcuni elementi della consapevolezza possono essere assenti, mentre altri sono presenti in alcuni casi meno frequenti.Parole chiave: (Auto-)coscienza; Teorie della coscienza di alto livello;  Teorie auto-rappresentazionali della coscienza; Fenomenicità; Teorie fenomenologiche della coscienz

The distribution of selected elements and minerals in soil of the conterminous United States

In 2007, the U.S. Geological Survey initiated a low-density (1 site per 1600 km2, 4857 sites) geochemical andmineralogical survey of soil of the conterminous United States as part of the North American Soil Geochemical Landscapes Project. Three soil samples were collected, if possible, from each site; (1) a sample from a depth of 0 to 5 cm, (2) a composite of the soil A-horizon, and (3) a deeper sample from the soil C-horizon or, if the top of the C-horizon was at a depth greater than 100 cm, from a depth of approximately 80–100 cm. The \u3c2 mm fraction of each sample was analysed for a suite of 45 major and trace elements following near-total multi-acid digestion. The major mineralogical components in samples from the soil A- and C-horizons were determined by a quantitative X-ray diffraction method using Rietveld refinement. Sampling ended in 2010 and chemical and mineralogical analyses were completed in May 2013.Maps of the conterminous United States showing predicted element and mineral concentrations were interpolated from actual soil data for each soil sample type by an inverse distance weighted (IDW) technique using ArcGIS software. Regional- and national-scale map patterns for selected elements and minerals apparent in interpolated maps are described here in the context of soil-forming factors and possible human inputs. These patterns can be related to (1) soil parent materials, for example, in the distribution of quartz, (2) climate impacts, for example, in the distribution of feldspar and kaolinite, (3) soil age, for example, in the distribution of carbonate in young glacial deposits, and (4) possible anthropogenic loading of phosphorus (P) and lead (Pb) to surface soil. This new geochemical and mineralogical data set for the conterminous United States represents a major step forward from prior national-scale soil geochemistry data and provides a robust soil data framework for the United States now and into the future

PATHOLOGICAL CHANGES IN 37 HUMAN RENAL HOMOTRANSPLANTS TREATED WITH IMMUNOSUPPRESSIVE DRUGS

Pathological changes in thirty‐seven human renal homotransplants are described. All the patients had been treated with Imuran, prednisone and actinomycin C; ten had also received local X‐irradiation to the transplant. Fifteen of the transplants were from patients in a rejection phase. Most of these kidneys were enlarged because of interstitial oedema and several were speckled with petechial hemorrhages. There was fibrinoid necrosis of afferent arterioles and interlobular arteries in twelve of the transplants, and the peritubular capillaries were disrupted in ten. Swelling of the arteriolar endothelial cells, fibrino‐platelet and fibrous intimal thickening of interlobular arteries were also common. In most of the transplants there was a light infiltration with small lymphocytes, plasma cells and a few larger pyroninophilic cells. Similar changes were present in the pelvis and ureter. Twelve of the transplants came from patients whose last rejection episode had been clinically reversed 14 to 117 days previously. AH these kidneys were enlarged because of compensatory hypertrophy. Seven showed some intimal thickening of the interlobular arteries and in three there was fibrinoid necrosis of arteriolar walls. Tubular atrophy, interstitial fibrosis and a light cellular infiltration were also common changes. Only one kidney appeared normal. Three transplants came from patients who had not experienced clinical evidence of a rejection episode. One showed acute tubular necrosis due to prolonged ischemia at the time of transplantation; one was almost normal; the third showed vascular lesions suggestive of old unrecognised rejection. Seven transplants had either not functioned or developed some complication necessitating their early removal. One of these was infarcted due to obstruction of the venous drainage; two showed massive acute tubular necrosis due to ischaemia; two, which were incompatible with their hosts on the basis of ABO blood groups, failed to excrete urine and showed distension of the arterioles and glomerular capillaries with erythrocytes; one bled uncontrollably from the pelvis; one came from a patient who died at twelve hours from hyperkalemia and hyponatremia during a massive post‐operative diuresis. This work was aided by grants A‐6283, A‐6344, HE‐07735, AM‐07772, AI‐01452, and OG‐27 from the U.S. Public Health Service, and by a grant from the Medical Research Council. The necropsies on cases described in this paper were either performed or supervised by Drs Coral Cotterall, Doris Courington, Carol Ewing, R. B. Hill, J. Jamroz, D. W. King, D. M. Lang, Martha La Via, Elizabeth Macintyre, N. McGrath, J. C. Maisel, C. G. Massion, D. R. Meekin, H. B. Neustein, S. Ryan, and D. E. Smith. We would like to thank all these pathologists for making this study possible. We are particularly grateful to Dr D. T. Rowlands, who supervised some of the necropsies, for his helpful co‐operation throughout this study. Expert assistance in preparing the sections and photomicrographs was given by Miss Jane Rendall. © 1965 BJU International Compan

ICOADS Release 3.0: a major update to the historical marine climate record

We highlight improvements to the International Comprehensive Ocean-Atmosphere Data Set (ICOADS) in the latest Release 3.0 (R3.0; covering 1662–2014). ICOADS is the most widely used freely available collection of surface marine observations, providing data for the construction of gridded analyses of sea surface temperature, estimates of air–sea interaction and other meteorological variables. ICOADS observations are assimilated into all major atmospheric, oceanic and coupled reanalyses, further widening its impact. R3.0 therefore includes changes designed to enable effective exchange of information describing data quality between ICOADS, reanalysis centres, data set developers, scientists and the public. These user-driven innovations include the assignment of a unique identifier (UID) to each marine report – to enable tracing of observations, linking with reports and improved data sharing. Other revisions and extensions of the ICOADS' International Maritime Meteorological Archive common data format incorporate new near-surface oceanographic data elements and cloud parameters. Many new input data sources have been assembled, and updates and improvements to existing data sources, or removal of erroneous data, made. Coupled with enhanced ‘preliminary’ monthly data and product extensions past 2014, R3.0 provides improved support of climate assessment and monitoring, reanalyses and near-real-time applications