Probing helium interfaces with light scattering : from fluid mechanics to statistical physics

We have investigated the formation of helium droplets in two physical situations. In the first one, droplets are atomised from superfluid or normal liquid by a fast helium vapour flow. In the second, droplets of normal liquid are formed inside porous glasses during the process of helium condensation. The context, aims, and results of these experiments are reviewed, with focus on the specificity of light scattering by helium. In particular, we discuss how, for different reasons, the closeness to unity of the index of refraction of helium allows in both cases to minimise the problem of multiple scattering and obtain results which it would not be possible to get using other fluids.Comment: 21 page

Exposure to solar ultraviolet radiation in young Dutch children: assessment by means of a 6-week retrospective questionnaire

Exposure to solar ultraviolet radiation in young Dutch children: assessment by means of a 6-week retrospective questionnaire. Termorshuizen F, Wijga A, Garssen J, Den Outer PN, Slaper H, Van Loveren H. Laboratory for Pathology and Immunobiology, National Institute of Public Health and the Environment, PO Box 1, Bilthoven 3720 BA, The Netherlands. We designed a 6-week retrospective questionnaire on sunlight exposure. Estimation of the short-term exposure to sunlight is important for observational human studies concerning the effects of ultraviolet radiation (UVR) on the human immune system and related resistance to infections. This questionnaire was given to the parents of 1672 1-year-old children in the Netherlands who participated in a birth cohort study. We evaluated the questionnaire and estimated the personal 6-week cumulative exposure to solar UVR. Only 910 questionnaires (54.4%) were filled out completely and consistently. This suggests that reporting data on children's outdoor exposure, even for the recent past, is often difficult. The data from these questionnaires indicated that the crude number of reported outdoor hours was enough to obtain a relative estimate of the individual exposure to ambient UVR, but that weighting for the effect of clothing was essential for the classification of the systemic UVR dosage received. Sunny weeks in the Netherlands in 1998, as were established by independent measurements of the levels of ambient UVR, vacations abroad, and sunburn, were associated with a comparatively high mean estimated exposure. These results support the suitability of the questionnaire for classifying the participants with respect to their short-term exposure to solar UVR

Comparison of satellite-derived UV irradiances with ground-based measurements at four European stations

Satellite-derived ultraviolet (UV) irradiances may form the basis for establishing a gloval UV climatology, provided that their accuracy is confirmed against ground-based measurements of known quality. In this study, quality-checked spectral UV irradiance measurements from four European stations (Sodankyla, Finland; Bilthoven, Netherlands; Ispra, Italy; and Thessaloniki, Greece) are compared with those derived from TOMS, based on the (version 8) data set. The aim of this study is to validate the TOMS UV irradiances and to investigate the origin of disagreements with ground-based data. Comparisons showed that TOMS overestimates summertime noon CIE-weighted irradiances from 6.6% at the high-latitude site of Sodankyla up to 19% for the three other sites. The influence of clouds and aerosols on the observed differences was investigated. For the other three sites (Bilthoven, Ispra, and Thessaloniki), TOMS overestimates the irradiance at 324 nm by almost 15% even under conditions with cloud optical depth of less than 5. For cloud-free days at Ispra and Thessaloniki, differences ranging between 3% and 20% are well correlated with aerosol optical depth. Copyright 2006 by the American Geophysical Union

Scientific Assessment of Ozone Depletion: 2010, Chapter 2 - Stratospheric Ozone and Surface Ultraviolet Radiation

As a result of the Montreal Protocol, ozone is expected to recover from the effect of ozone-depleting substances (ODSs) as their abundances decline in the coming decades. The 2006 Assessment showed that globally averaged column ozone ceased to decline around 1996, meeting the criterion for the first stage of recovery. Ozone is expected to increase as a result of continued decrease in ODSs (second stage of recovery). This chapter discusses recent observations of ozone and ultraviolet radiation in the context of their historical records. Natural variability, observational uncertainty, and stratospheric cooling necessitate a long record in order to attribute an ozone increase to decreases in ODSs. The primary tools used in this Assessment for prediction of ozone are chemistry-climate models (CCMs). These CCMs are designed to represent the processes determining the amount of stratospheric ozone and its response to changes in ODSs and greenhouse gases. Eighteen CCMs have been recently evaluated using a variety of process-based compari-sons to measurements. The CCMs are further evaluated here by comparison of trends calculated from measurements with trends calculated from simulations designed to reproduce ozone behavior during an observing period