scholarly journals COST Lecture 2019 AE GM Barcelona: International Network to Encourage the Use of Monitoring and Forecasting Dust Products (InDust)

2020 ◽  
pp. 1-15
Author(s):  
Anca Nemuc ◽  
Sara Basart ◽  
Aurelio Tobias ◽  
Slobodan Nickovic ◽  
Francesca Barnaba ◽  
...  
Keyword(s):  
Service Providers ◽  
Mineral Dust ◽  
Dust Storms ◽  
Dust Particles ◽  
Economic Sectors ◽  
International Network ◽  
Airborne Dust ◽  
Monitoring And Forecasting ◽  
High Concentrations ◽  
Research Networking

Amongst the most significant extreme meteorological phenomena are the Sand and Dust Storms (SDS). Owing to significant amounts of airborne mineral dust particles generated during these events, SDS have impacts on climate, the environment, human health, and many socio-economic sectors (e.g. aviation, solar energy management). Many studies and reports have underlined that the society has to understand, manage and mitigate the risks and effects of SDS on life, health, property, the environment and the economy in a more unified way. The EU-funded European Cooperation in Science and Technology (COST) Action ‘InDust: International network to encourage the use of monitoring and forecasting Dust products’ has an overall objective to establish a network involving research institutions, service providers and potential end users on airborne dust information. We are a multidisciplinary group of international experts on aerosol measurements, aerosol modelling, stakeholders and social scientists working together, exchanging ideas to better coordinate and harmonize the process of transferring dust observation and prediction data to users, as well as to assist the diverse socio-economic sectors affected by the presence of high concentrations of airborne mineral dust. This article highlights the importance of being actively engaged in research networking activities, supported by EU and COST actions since common efforts help not only each scientist by shaping their expertise and strengthening their position, but also all communities.

inDust: International Network to encourage the use of monitoring and forecasting DUST products

2020 ◽  
Author(s):  
Sara Basart ◽  
Slodoban Nickovic ◽  
Keyword(s):  
Air Quality ◽  
Solar Energy ◽  
Significant Role ◽  
Service Providers ◽  
Early Warning Systems ◽  
End Users ◽  
Dust Storms ◽  
Dust Particles ◽  
Accurate Information ◽  
Economic Sectors

<p>Sand and Dust Storms (SDS) are extreme meteorological phenomena that generate significant amounts of airborne mineral dust particles. SDS plays a significant role in different aspects of weather, climate and atmospheric chemistry. Also, SDS represents a severe hazard for life, health, property, environment and economy, which is aligned with several Sustainable Developed Goal (SDG) targets established by the United Nations (UN). Understanding, managing, and mitigating SDS risks and effects requires fundamental and cross-disciplinary knowledge.</p><p>Over the last few years, there is an increasing need for SDS accurate information and predictions to support early warning systems, and preparedness and mitigation plans in addition to growing interest from diverse stakeholders, such as solar energy plant managers, health professionals, aviation and policymakers from environmental and health public sectors. Current attempts to transfer tailored products to end-users are not coordinated, and the same technological and social obstacles are tackled individually by all different groups, a process that makes the use of data slow and expensive.</p><p>The EU-funded COST Action inDust (www.cost-indust.eu, CA16202) has an overall objective to establish a network involving research institutions, service providers and potential end-users of information on airborne dust that can assist the diverse socio-economic sectors affected by the presence of high concentrations of atmospheric dust. In line with this main objective, the network is being worked on the identification and engagement of representatives of dust affected socio-economic sectors (targeting on air quality and health, aviation and solar energy) from different countries in Europe but also in North Africa and the Middle East. Moreover, the participation of South African, American and importantly Asian partners brings the possibility of extending the application of the developed products, protocols and tools well beyond the European borders, including areas like Asian regions where dust particles play a significant role in the air quality and meteorological processes.</p><p>The primary outcomes of the network are the identification of the needs of the various and new dust-related products and services able to satisfy these needs. As a result, the network has been working on a dust catalogue which includes an overview of (ground-based and satellite) observations and model products.</p>

Saharan Dust Records and Its Impact in the European Alps

2021 ◽  
Author(s):  
Marion Greilinger ◽  
Anne Kasper-Giebl
Keyword(s):  
Mineral Dust ◽  
Cloud Condensation Nuclei ◽  
Ice Cores ◽  
Atmospheric Particulate Matter ◽  
Saharan Dust ◽  
Cloud Formation ◽  
Dust Particles ◽  
European Alps ◽  
Airborne Dust ◽  
Dust Events

Mineral dust is one of the main natural sources of atmospheric particulate matter, with the Sahara being one of the most important source regions for the occurrence and deposition of mineral dust in Europe. The occurrence of dust events in the European Alps is documented via measurements of airborne dust and its deposits onto the glaciers. Dust events occur mainly in spring, summer, and early autumn. Dust layers are investigated in ice cores spanning the last millennium as well as in annual snow packs. They strongly affect the overall flux of dust-related compounds (e.g., calcium and magnesium), provide an alkaline input to wet deposition chemistry, and change the microbial abundance and diversity of the snow pack. Still airborne mineral dust particles can act as ice nuclei and cloud condensation nuclei, influencing the formation of cloud droplets and hence cloud formation and precipitation. Dust deposits on the snow lead to a darkening of the surface, referred to as “surface albedo reduction,” which influences the timing of the snowmelt and reduces the annual mass balance of glaciers, showing a direct link to glacier retreat as observed presently in a warming climate.

scholarly journals Feedback between dust particles and atmospheric processes over West Africa during dust episodes in March 2006 and June 2007

2010 ◽  
Vol 10 (22) ◽  
pp. 10771-10788 ◽  
Author(s):  
T. Stanelle ◽  
B. Vogel ◽  
H. Vogel ◽  
D. Bäumer ◽  
C. Kottmeier
Keyword(s):  
West Africa ◽  
Mineral Dust ◽  
Dust Storms ◽  
Dust Particles ◽  
Total Emission ◽  
Radiative Effect ◽  
Radiative Fluxes ◽  
Dust Layer ◽  
Emission Fluxes ◽  
The Impact

Abstract. We used the comprehensive model system COSMO-ART to quantify the impact of mineral dust on the radiative fluxes, the temperature and the feedback between dust particles and their emissions. We simulated two dust storms over West Africa in March 2006 and in June 2007. Simulations with and without coupling of the actual dust concentration with the radiative fluxes and the thermodynamics were carried out for each case. The model results for the 2006 case were compared with observations of the AMMA campaign. At the surface the shortwave radiative effect of mineral dust can be described by a linear relation between the changes in net surface radiation and the aerosol optical depth (AOD). For an AOD at 450 nm of 1 the average shortwave radiation reduction amounts −140 W m−2 during noon. The longwave radiative effect of mineral dust is nonlinear, with an average increase of +70 W m−2 for an AOD (450 nm) of 1. At the top of the atmosphere the effect of the dust layer with an AOD of 1 on radiative fluxes is not as significant as at the surface. It is slightly positive for the shortwave and approximately 26 W m−2 for the longwave radiation. The height range and the extension of the dust layer determine the effect of dust particles on the 2 m temperature. When the dust layer is attached to the surface and lasts for several days it leads to an increase of the surface temperature even during daytime. In case of an elevated dust layer there is a decrease in 2 m temperature of up to 4 K during noon. It is shown, that the temperature changes caused by mineral dust may result in horizontal temperature gradients which also modify near surface winds. Since surface wind thresholds decide the uptake of dust from the surface, a feedback on total emission fluxes is established. The coupled model provides an increase in the total emission fluxes of dust particles by about 16% during the dust storm in March 2006 and 25% during the dust episode in June 2007.

scholarly journals Technical Note: Minerals in dust productive soils – impacts and global distribution

2011 ◽  
Vol 11 (9) ◽  
pp. 26009-26034 ◽  
Author(s):  
S. Nickovic ◽  
A. Vukovic ◽  
M. Vujadinovic ◽  
V. Djurdjevic ◽  
G. Pejanovic
Keyword(s):  
High Resolution ◽  
Mineral Composition ◽  
Atmospheric Transport ◽  
Dust Emission ◽  
Technical Note ◽  
Dust Storms ◽  
Dust Particles ◽  
Atmospheric Conditions ◽  
Airborne Dust ◽  
Aerosol Process

Abstract. Dust storms and associated mineral aerosol transport are mainly driven by meso and synoptic scale atmospheric processes. It is therefore essential that the dust aerosol process and background atmospheric conditions that drive the dust emission and atmospheric transport be represented with sufficiently well resolved spatial and temporal features. Effects of airborne dust interactions with the environment are determent by the mineral composition of dust particles. Fractions of various minerals in the aerosol are determined by the mineral composition of arid soils, therefore high-resolution specification of mineral and physical properties of dust sources is needed as well. Most current dust atmospheric models simulate/predict the evolution of dust concentration but in most cases they do not consider fractions of minerals in dust. Accumulated knowledge on impacts of mineral composition in dust on weather and climate processes emphasizes the importance of considering minerals in modelling systems. Following such needs, in this study we developed a global dataset on mineral composition of potentially dust productive soils. In our study (a) we mapped mineral data into a high-resolution 30-s grid, (b) we included mineral carrying soil types in dust productive regions that were not considered in previous studies, and (c) included phosphorus having in mind their importance for terrestrial and marine nutrition processes.

Tropospheric Mineral Dust Study by High Spectral Resolution Infrared Satellite during intense dust storms

2021 ◽  
Author(s):  
Perla Alalam ◽  
Hervé Herbin
Keyword(s):  
Mineral Dust ◽  
Complex Refractive Index ◽  
Estimation Method ◽  
Dust Storms ◽  
High Spectral Resolution ◽  
Dust Particles ◽  
Physical Parameters ◽  
Chemical Compositions ◽  
Storm Events ◽  
Atmospheric Measurements

<p>Large desert lands such as Sahara, Gobi or Australia present main sources of atmospheric mineral dust caused by intense dust storms. Transported dust particles undergo physical and chemical changes affecting their microphysical and optical properties. This modifies their scattering and absorption properties and alters the global atmospheric radiative budget.</p><p>Currently, remote sensing techniques represent a powerful tool for quantitative atmospheric measurements and the only means of analyzing its evolution from local to global scale. In order to improve the knowledge of atmospheric aerosol distributions, many efforts were made particularly in the development of hyperspectral infrared spectrometers and processing algorithms. However, to fully exploit these measurements, a perfect knowledge of Complex Refractive Index (CRI) is required.</p><p>In that purpose, a new methodology <sup></sup>based on laboratory measurements of mineral dust in suspension coupled with an optimal estimation method has been developed. This approach allows getting access to CRI of several desert samples with various chemical compositions.</p><p>Here, we present the first results of the physical parameters (effective radius and concentration) retrievals using Infrared Atmospheric Sounding Interferometer IASI data, during dust storm events. The latter use the CRI of different desert samples obtained in laboratory and a new radiative transfer algorithm (ARAHMIS) developed at Laboratoire d’Optique Atmosphérique LOA.</p>

Influence of chemical aging on physico-chemical properties of mineral dust particles: A case study of 2016 dust storms over Delhi

2020 ◽  
Vol 267 ◽  
pp. 115338
Author(s):  
Vikas Goel ◽  
Sumit K. Mishra ◽  
Prabir Pal ◽  
Ajit Ahlawat ◽  
Narayanasamy Vijayan ◽  
...  
Keyword(s):  
Mineral Dust ◽  
Chemical Properties ◽  
Dust Storms ◽  
Dust Particles ◽  
Chemical Aging ◽  
Physico Chemical

A comparative evaluation of water uptake on several mineral dust sources

2010 ◽  
Vol 7 (2) ◽  
pp. 162 ◽  
Author(s):  
Juan G. Navea ◽  
Haihan Chen ◽  
Min Huang ◽  
Gregory R. Carmichel ◽  
Vicki H. Grassian
Keyword(s):  
Chemical Composition ◽  
Relative Humidity ◽  
Dust Particle ◽  
Water Uptake ◽  
Mineral Dust ◽  
Dust Storms ◽  
Dust Aerosol ◽  
Dust Particles ◽  
Particle Interactions ◽  
Dust Sources

Environmental context. Dust particles produced from wind blown soils are of global significance as these dust particles not only impact visibility, as evident in the recent 2009 Australian dust storm, but also atmospheric chemistry, climate and biogeochemical cycles. The amount of water vapour in the atmosphere (relative humidity) can play a role in these global processes yet there are few studies and little quantitative data on water-dust particle interactions. The focus of this research is on quantifying water-dust particle interactions for several dust sources including Asia and Africa where dust storms are most prevalent. Abstract. Mineral dust aerosol provides a reactive surface in the troposphere. The reactivity of mineral dust depends on the source region as chemical composition and mineralogy of the aerosol affects its interaction with atmospheric gases. Furthermore, the impact of mineral dust aerosol in atmospheric processes and climate is a function of relative humidity. In this study, we have investigated water uptake of complex dust samples. In particular, water uptake as a function of relative humidity has been measured on three different dust sources that have been characterised using a variety of bulk and surface techniques. For these well-characterised dust samples, it is shown that although there are variations in chemical composition and mineralogy, on a per mass basis, water uptake capacities for the three dusts are very similar and are comparable to single component clay samples. These results suggest that the measured uptake of water of these bulk samples is dominated by the clay component.

scholarly journals Analysis of airborne dust effects on terrestrialmicrowave propagation in arid area

2019 ◽  
Vol 8 (3) ◽  
pp. 1014-1021
Author(s):  
Elfatih A. A. Elsheikh ◽  
Islam Md. Rafiqul ◽  
Mohamad Hadi Habaebi ◽  
Ahmad F. Ismail ◽  
Z. E. O. Elshaikh ◽  
...  
Keyword(s):  
Dust Storm ◽  
Electromagnetic Waves ◽  
Dust Storms ◽  
Dust Particles ◽  
Cross Polarization ◽  
Airborne Dust ◽  
Millimeter Wave Propagation ◽  
Suspended Dust ◽  
Storm Characteristics ◽  
Dust Effects

Sand and dust storms are environmental phenomena ,during these storms optical visibility might be decreased, consequently, atmospheric attenuation is clearly noticed.Micro-wave (MW) and Milimeter-wave (mm) propagation is severely affected by dust and sand storms in considerable areas around the world. Suspended dust particles may directly cause attenuation and cross polarization to the Electromagnetic waves propagating through the storm. In this paper, a thorough investigation of dust storm characteristics based onmeasured optical visibility and relative humidity is presented. In addition,the dust storms effects of on Micro-wave and Millimeter-wave propagation have been studied based on data measured Received Signal levels (RSL)and dust storm characteristics synchronously. Analyticaldustattenuationmodels predictions are matched to the measured attenuationdata at 14 GHz and 21 GHz. It has been found that the measured attenuation is approximately ten times higher than the predicted attenuation for both frequencies.

A modeling insight into the transport of large dust particles

2021 ◽  
Author(s):  
Eleni Drakaki ◽  
Alexandra Tsekeri ◽  
Vasillis Amiridis ◽  
Stavros Solomos ◽  
Antonis Gkikas ◽  
...  
Keyword(s):  
Size Distribution ◽  
Mineral Dust ◽  
Saharan Dust ◽  
Cloud Formation ◽  
Dust Particles ◽  
Negative Effects ◽  
Airborne Dust ◽  
Horizon 2020 ◽  
Research And Innovation ◽  
The Impact

<p>Mineral dust is an important component of the climate system, affecting radiation, cloud formation, biogeochemical cycles, as well as having negative effects on solar energy budget and human health. All these processes are affected from the size of the particles which is significantly underestimated by the Earth System Models. Here, we present results from a first attempt to modify the size distribution parameterizations in the GOCART-AFWA dust scheme of WRF - Chem, by including the large dust particles with diameters greater than 20 µm to describe the mineral dust cycle. The parameterization is based on Saharan dust observational datasets from FENNEC and SAMUM campaigns. We investigate the impact of the extended size distribution on the overall transported dust load and also the impact of particle settling considerations in deposition rates. The model results are compared with airborne dust measurements from AER-D campaign. In order to achieve the best agreement with the observations, an artificial force that counteracts gravity approximately by 80% for the large particles is needed, indicating the presence of one or more under-represented physical processes in the model.</p><p><strong>Acknowledgment:</strong> This research was supported by D-TECT (Grant Agreement 725698) funded by the European Research Council (ERC) under the European Union's Horizon 2020 research and innovation programme. </p>

scholarly journals Temporal analysis of Sand and Dust Storms (SDS) between the years 2003 and 2017 in the Central Asia

2019 ◽  
Vol 99 ◽  
pp. 02004
Author(s):  
Cihan Dundar ◽  
Ayse Gokcen Isik ◽  
Kahraman Oguz
Keyword(s):  
Middle East ◽  
Central Asia ◽  
Energy Budget ◽  
Fine Particles ◽  
Mineral Dust ◽  
Temporal Analysis ◽  
Vital Role ◽  
Dust Storms ◽  
Dust Particles ◽  
East Region

Mineral dust particles play a vital role in climate and the Earth's energy budget and can have impact on weather systems. It has both direct (dust-radiation effect) and indirect (dust-microphysical effect) impacts on the energy budget effect. The most important sources of dust aerosols are located in the Northern Hemisphere, primarily over the Sahara in North Africa, the Middle East, Central and South Asia respectively and Central Asia is under the influence of mineral dust. The objective of this study to carry out intensity and frequency analysis of sand and dust storm in Central Asia for the period 2003-2017 and compare the results with global values as well as the values of the Middle East region. The AOD and AE parameters can be used to differentiate between coarse and fine particles of aerosols. To investigate average annual and monthly AOD (aerosol optical depth) and AE (angstrom exponent) for the period 2003-2017, AOD and AE data of MODIS Aqua is obtained from Giovanni website. In summary, for the last years (2013-2017), annual mean AOD is comparably lower than the other periods while the values are the highest between 2008 and 2012 for both Central Asia and Middle East. The results point out that there is no increasing trend in AOD values for the recent years and annual Central Asia AOD values show a similar trend with the Middle East AOD values.

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