111 research outputs found
\u201cGive, but Give until It Hurts\u201d: The Modulatory Role of Trait Emotional Intelligence on the Motivation to Help
Two studies investigated the effect of trait Emotional Intelligence (trait EI) on people\u2019s moti- vation to help. In Study 1, we developed a new computer-based paradigm that tested partic- ipants\u2019 motivation to help by measuring their performance on a task in which they could gain a hypothetical amount of money to help children in need. Crucially, we manipulated partici- pants\u2019 perceived efficacy by informing them that they had been either able to save the chil- dren (positive feedback) or unable to save the children (negative feedback). We measured trait EI using the Trait Emotional Intelligence Questionnaire\u2013Short Form (TEIQue-SF) and assessed participants\u2019 affective reactions during the experiment using the PANAS-X. Results showed that high and low trait EI participants performed differently after the presen- tation of feedback on their ineffectiveness in helping others in need. Both groups showed increasing negative affective states during the experiment when the feedback was negative; however, high trait EI participants better managed their affective reactions, modulating the impact of their emotions on performance and maintaining a high level of motivation to help. In Study 2, we used a similar computerized task and tested a control situation to explore the effect of trait EI on participants\u2019 behavior when facing failure or success in a scenario unre- lated to helping others in need. No effect of feedback emerged on participants\u2019 emotional states in the second study. Taken together our results show that trait EI influences the impact of success and failure on behavior only in affect-rich situation like those in which people are asked to help others in need
Four-dimensional distribution of the 2010 Eyjafjallajökull volcanic cloud over Europe observed by EARLINET
© Author(s) 2013. This work is distributed under the Creative Commons Attribution 3.0 License.The eruption of the Icelandic volcano Eyjafjallaj ökull in April-May 2010 represents a "natural experiment" to study the impact of volcanic emissions on a continental scale. For the first time, quantitative data about the presence, altitude, and layering of the volcanic cloud, in conjunction with optical information, are available for most parts of Europe derived from the observations by the European Aerosol Research Lidar NETwork (EARLINET). Based on multi-wavelength Raman lidar systems, EARLINET is the only instrument worldwide that is able to provide dense time series of high-quality optical data to be used for aerosol typing and for the retrieval of particle microphysical properties as a function of altitude. In this work we show the four-dimensional (4-D) distribution of the Eyjafjallajökull volcanic cloud in the troposphere over Europe as observed by EARLINET during the entire volcanic event (15 April-26 May 2010). All optical properties directly measured (backscatter, extinction, and particle linear depolarization ratio) are stored in the EARLINET database available at www.earlinet.org. A specific relational database providing the volcanic mask over Europe, realized ad hoc for this specific event, has been developed and is available on request at www.earlinet.org. During the first days after the eruption, volcanic particles were detected over Central Europe within a wide range of altitudes, from the upper troposphere down to the local planetary boundary layer (PBL). After 19 April 2010, volcanic particles were detected over southern and south-eastern Europe. During the first half of May (5-15 May), material emitted by the Eyjafjallajökull volcano was detected over Spain and Portugal and then over the Mediterranean and the Balkans. The last observations of the event were recorded until 25 May in Central Europe and in the Eastern Mediterranean area. The 4-D distribution of volcanic aerosol layering and optical properties on European scale reported here provides an unprecedented data set for evaluating satellite data and aerosol dispersion models for this kind of volcanic events.Peer reviewe
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EARLINET observations of the 14-22-May long-range dust transport event during SAMUM 2006: Validation of results from dust transport modelling
We observed a long-range transport event of mineral dust from North Africa to South Europe during the Saharan Mineral
Dust Experiment (SAMUM) 2006. Geometrical and optical properties of that dust plume were determined with Sun
photometer of the Aerosol Robotic Network (AERONET) and Raman lidar near the North African source region, and
with Sun photometers of AERONET and lidars of the European Aerosol Research Lidar Network (EARLINET) in the
far field in Europe. Extinction-to-backscatter ratios of the dust plume over Morocco and Southern Europe do not differ.
Ångstr¨om exponents increase with distance from Morocco. We simulated the transport, and geometrical and optical
properties of the dust plume with a dust transport model. The model results and the experimental data show similar
times regarding the appearance of the dust plume over each EARLINET site. Dust optical depth from the model agrees
in most cases to particle optical depth measured with the Sun photometers. The vertical distribution of the mineral dust
could be satisfactorily reproduced, if we use as benchmark the extinction profiles measured with lidar. In some cases
we find differences. We assume that insufficient vertical resolution of the dust plume in the model calculations is one
reason for these deviations
Experimental techniques for the calibration of lidar depolarization channels in EARLINET
Particle depolarization ratio retrieved from lidar measurements are commonly used for aerosol-typing studies, microphysical inversion, or mass concentration retrievals. The particle depolarization ratio is one of the primary parameters that can differentiate several major aerosol components but only if the measurements are accurate enough. The accuracy related to the retrieval of particle depolarization ratios is the driving factor for assessing and improving the uncertainties of the depolarization products. This paper presents different depolarization calibration procedures used to improve the quality of the depolarization data. The results illustrate a significant improvement of the depolarization lidar products for all the selected lidar stations that have implemented depolarization calibration procedures. The calibrated volume and particle depolarization profiles at 532 nm show values that fall within a range that is generally accepted in the literature
Representativeness of aerosol measurements: EARLINET-CALIPSO correlative study
The high variability of tropospheric aerosols, both in
space and time, is the main cause of the high uncertainty
about radiative forcing related to tropospheric aerosols
and their interaction with clouds. Because of the lack of
high resolution aerosol global vertical profiles, the
vertical mixing has not been considered so far in studies
of spatial and temporal variability. The CALIPSO
mission provides the first opportunity to investigate the
4-D aerosol and cloud fields in detail. However, because
of the CALIOP small footprint and the revisit time of 16
days, correlative ground-based lidar observations are
necessary in order to investigate the representativeness
of these satellite observations. EARLINET, the
European Aerosol Research Lidar Network, started
correlative measurements for CALIPSO in June 2006,
right after the CALIPSO launch. An integrated study of
CALIPSO and EARLINET correlative measurements
opens new possibilities for spatial (both horizontal and
vertical) and temporal representativeness investigation
of polar-orbit satellite measurements also in terms of
revisit time.Postprint (published version
Individual and school level correlates of moderate to vigorous physical activity among school-children in Germany – a multi-level analysis
Long-term aerosol and cloud database from correlative EARLINET-CALIPSO observations
The European Aerosol Research Lidar Network,
EARLINET, performs correlative observations during
CALIPSO overpasses based on a sophisticated measurement
strategy since June 2006. Within a dedicated
activity supported by the European Space Agency
(ESA), sixteen EARLINET stations contributed about
1500 measurements during an intensive observational
period from May 2008 to October 2009. From these
measurements, we establish a long-term aerosol and
cloud database of correlative EARLINET-CALIPSO
observations. This database shall provide a basis for
homogenizing long-term space-borne observations
conducted with different lidar instruments operating
at different wavelengths on various platforms over the
next decade(s). The database is also used to study the
quality and representativeness of satellite lidar cross
sections along an orbit against long-term lidar network
observations on a continental scale.Postprint (published version
EARLINET instrument intercomparison campaigns: overview on strategy and results
This paper introduces the recent European Aerosol Research Lidar Network (EARLINET) quality-assurance efforts at instrument level. Within two dedicated campaigns and five single-site intercomparison activities, 21 EARLINET systems from 18 EARLINET stations were intercompared between 2009 and 2013. A comprehensive strategy for campaign setup and data evaluation has been established. Eleven systems from nine EARLINET stations participated in the EARLINET Lidar Intercomparison 2009 (EARLI09). In this campaign, three reference systems were qualified which served as traveling standards thereafter. EARLINET systems from nine other stations have been compared against these reference systems since 2009. We present and discuss comparisons at signal and at product level from all campaigns for more than 100 individual measurement channels at the wavelengths of 355, 387, 532, and 607¿nm. It is shown that in most cases, a very good agreement of the compared systems with the respective reference is obtained. Mean signal deviations in predefined height ranges are typically below ±2¿%. Particle backscatter and extinction coefficients agree within ±2¿¿×¿¿10-4¿km-1¿sr-1 and ±¿0.01¿km-1, respectively, in most cases. For systems or channels that showed larger discrepancies, an in-depth analysis of deficiencies was performed and technical solutions and upgrades were proposed and realized. The intercomparisons have reinforced confidence in the EARLINET data quality and allowed us to draw conclusions on necessary system improvements for some instruments and to identify major challenges that need to be tackled in the future.Peer ReviewedPostprint (published version
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