Modeling lightning-NOx chemistry on a sub-grid scale in a global chemical transport model

For the first time, a plume-in-grid approach is implemented in a chemical transport model (CTM) to parameterize the effects of the nonlinear reactions occurring within high concentrated NO_<i>x</i> plumes from lightning NO_<i>x</i> emissions (LNO_<i>x</i>) in the upper troposphere. It is characterized by a set of parameters including the plume lifetime, the effective reaction rate constant related to NO_<i>x</i>–O₃ chemical interactions, and the fractions of NO_<i>x</i> conversion into HNO₃ within the plume. Parameter estimates were made using the Dynamical Simple Model of Atmospheric Chemical Complexity (DSMACC) box model, simple plume dispersion simulations, and the 3-D Meso-NH (non-hydrostatic mesoscale atmospheric model). In order to assess the impact of the LNO_<i>x</i> plume approach on the NO_<i>x</i> and O₃ distributions on a large scale, simulations for the year 2006 were performed using the GEOS-Chem global model with a horizontal resolution of 2° × 2.5°. The implementation of the LNO_<i>x</i> parameterization implies an NO_<i>x</i> and O₃ decrease on a large scale over the region characterized by a strong lightning activity (up to 25 and 8 %, respectively, over central Africa in July) and a relative increase downwind of LNO_<i>x</i> emissions (up to 18 and 2 % for NO_<i>x</i> and O₃, respectively, in July). The calculated variability in NO_<i>x</i> and O₃ mixing ratios around the mean value according to the known uncertainties in the parameter estimates is at a maximum over continental tropical regions with ΔNO_<i>x</i> [−33.1, +29.7] ppt and ΔO₃ [−1.56, +2.16] ppb, in January, and ΔNO_<i>x</i> [−14.3, +21] ppt and ΔO₃ [−1.18, +1.93] ppb, in July, mainly depending on the determination of the diffusion properties of the atmosphere and the initial NO mixing ratio injected by lightning. This approach allows us (i) to reproduce a more realistic lightning NO_<i>x</i> chemistry leading to better NO_<i>x</i> and O₃ distributions on the large scale and (ii) to focus on other improvements to reduce remaining uncertainties from processes related to NO_<i>x</i> chemistry in CTM

Caractérisation et modélisation sous-maille des panaches d'éclairs : implication sur le bilan de l'ozone et les espèces azotées de la haute troposphère

Les éclairs représentent une des sources majeures d'oxydes d'azote (N Ox = N O + N O2 ) dans la haute troposphère. Ces émissions locales sont à l'origine de fortes concentrations de NOx, dont le temps de vie est augmenté dans cette partie de l'atmosphère, et sont associées à des panaches transportés à l'échelle intercontinentale. Aussi, l'importance des émissions par les éclairs pour la chimie de la haute troposphère et notamment pour la production d'ozone et la capacité oxydante de l'atmosphère n'est plus a prouver. Mon travail de thèse est dédié à la caractérisation des panaches de NOx issus des éclairs et la modélisation sous-maille associée afin de déterminer leur impact sur le bilan de l'ozone et les espèces azotées de la haute troposphère. L'analyse des mesures in-situ du programme aéroporté MOZAIC, dans les moyennes latitudes nord, couplées aux calculs du modèle lagrangien FLEXPART, et aux observations au sol et depuis l'espace des flashs d'éclairs et des nuages est réalisée. Cette étude met en évidence l'existence des panaches très étendus de N Oy issus des émissions d'éclairs et rend compte de leur fréquence, leur composition et leur évolution chimique au cours du transport. Un gradient négatif (positif) de NOy (O3) est mesuré dans les panaches de -0,4 (+18) ppbv de différence, pendant le printemps et -0,6 (+14) ppbv de différence, en été, entre l'Amérique du Nord et l'Europe. De plus, pour la première fois, une paramétrisation de panache associée aux émissions d'éclairs est implémentée dans un CTM. Cette approche permet le transport des effets de la chimie non-linéaire ayant lieu dans les panaches et conduit à une diminution significative des NOx et de l'O3 dans les régions caractérisées par une activité électrique électrique intense (-25 % et -8%, respectivement, en Afrique Centrale, en juillet) et une augmentation dans le vent des émissions (+10 % et +1 %, respectivement, sur l'Océan Atlantique, en juillet). Ces travaux permettent ainsi de réduire les incertitudes sur la représentation de ces processus non-linéaires et à une échelle plus petite que celle de la maille des modèles en vue d'une meilleure estimation (i) des distributions d'oxydes d'azote liées aux éclairs et (ii) de la production d'ozone associée à l'échelle globale.Lightning emissions are one of the most important sources of nitrogen oxides (NOx = NO+NO2 ) in the upper troposphere. They imply high N Ox concentrations where their lifetime is longer in this part of the atmosphere and can be associated to large plumes transported over long distance. Furthermore, the decisive role of lightning emissions in the upper tropospheric chemistry and especially on the ozone production and the oxidizing capacity of the atmosphere is well known. My PhD is dedicated to the characterization of the lightning-NOx related plumes and the associated sub-grid modeling in order to determine their impact on the ozone and nitrogen oxyde burden in the upper troposphere. The analysis of the MOZAIC measurements in the northern-mid-latitudes coupled with FLEXPART Lagrangian model calculations, ground and space-based observations of lightning flashes and clouds is made. This study highlights the existence of large scale plumes of NOy from lightning emissions and describes their frequency, their chemical composition and evolution during the long-range transport. A negative (positive) gradient of NOy (O3) is found within the large scale plumes of about -0.4(+18) ppbv difference, during spring, and -0.6(+14) ppbv difference, in summer, between North America and Europe. Therefore, for the first time, a plume parameterization for lightning NOx emissions is implemented into CTM. This approach allows the transport of the non-linear chemistry effects occurring within plumes. The implementation of the plume-in-grid parameterization leads to a significant NOx and O3 decrease over the region characterized by a strong lightning activity (up to -25 % and -8 %, respectively, over Central Africa, in July) and a relative increase downwind of lightning NOx emissions (up to +10 % and +1 %, respectively, over Atlantic ocean, in July). This work allows to reduce the uncertainties on the representation of the non-linear processes at a smaller scale than the model grid in order to provide better estimates of (i) the nitrogen oxide distribution related to lightning and (ii) the associated ozone production at the large scale

Pea Albumin 1 Subunit b (PA1b), a Promising Bioinsecticide of Plant Origin

PA1b (Pea Albumin 1, subunit b) is a peptide extract from pea seeds showing significant insecticidal activity against certain insects, such as cereal weevils (genus Sitophilus), the mosquitoes Culex pipiens and Aedes aegyptii, and certain species of aphids. PA1b has great potential for use on an industrial scale and for use in organic farming: it is extracted from a common plant; it is a peptide (and therefore suitable for transgenic applications); it can withstand many steps of extraction and purification without losing its activity; and it is present in a seed regularly consumed by humans and mammals without any known toxicity or allergenicity. The potential of this peptide to limit pest damage has stimulated research concerning its host range, its mechanism of action, its three-dimensional structure, the natural diversity of PA1b and its structure-function relationships

Acceleration of global N₂O emissions seen from two decades of atmospheric inversion

Nitrous oxide (N2O) is the third most important long-lived GHG and an important stratospheric ozone depleting substance. Agricultural practices and the use of N-fertilizers have greatly enhanced emissions of N2O. Here, we present estimates of N2O emissions determined from three global atmospheric inversion frameworks during the period 1998–2016. We find that global N2O emissions increased substantially from 2009 and at a faster rate than estimated by the IPCC emission factor approach. The regions of East Asia and South America made the largest contributions to the global increase. From the inversion-based emissions, we estimate a global emission factor of 2.3 ± 0.6%, which is significantly larger than the IPCC Tier-1 default for combined direct and indirect emissions of 1.375%. The larger emission factor and accelerating emission increase found from the inversions suggest that N2O emission may have a nonlinear response at global and regional scales with high levels of N-input

Modeling lightning-NOx chemistry at sub-grid scale in a global chemical transport model

For the first time, a plume-in-grid approach is implemented in a chemical transport model (CTM) to parameterize the effects of the non-linear reactions occurring within high concentrated NOx plumes from lightning NOx emissions (LNOx) in the upper troposphere. It is characterized by a set of parameters including the plume lifetime, the effective reaction rate constant related to NOx-O3 chemical interactions and the fractions of NOx conversion into HNO3 within the plume. Parameter estimates were made using the DSMACC chemical box model, simple plume dispersion simulations and the mesoscale 3-D Meso-NH model. In order to assess the impact of the LNOx plume approach on the NOx and O3 distributions at large scale, simulations for the year 2006 were performed using the GEOS-Chem global model with a horizontal resolution of 2° × 2.5°. The implementation of the LNOx parameterization implies NOx and O3 decrease at large scale over the region characterized by a strong lightning activity (up to 25 and 8 %, respectively, over Central Africa in July) and a relative increase downwind of LNOx emissions (up to 18 and 2 % for NOx and O3, respectively, in July) are derived. The calculated variability of NOx and O3 mixing ratios around the mean value according to the known uncertainties on the parameter estimates is maximum over continental tropical regions with ΔNOx [−33.1; +29.7] ppt and ΔO3 [−1.56; +2.16] ppb, in January, and ΔNOx [−14.3; +21] ppt and ΔO3 [−1.18; +1.93] ppb, in July, mainly depending on the determination of the diffusion properties of the atmosphere and the initial NO mixing ratio injected by lightning. This approach allows (i) to reproduce a more realistic lightning NOx chemistry leading to better NOx and O3 distributions at the large scale and (ii) focus on other improvements to reduce remaining uncertainties from processes related to NOx chemistry in CTM

High toxicity and specificity of the saponin 3-GlcA-28-AraRhaxyl-medicagenate, from Medicago truncatula seeds, for Sitophilus oryzae

<p>Abstract</p> <p>Background</p> <p>Because of the increasingly concern of consumers and public policy about problems for environment and for public health due to chemical pesticides, the search for molecules more safe is currently of great importance. Particularly, plants are able to fight the pathogens as insects, bacteria or fungi; so that plants could represent a valuable source of new molecules.</p> <p>Results</p> <p>It was observed that <it>Medicago truncatul</it>a seed flour displayed a strong toxic activity towards the adults of the rice weevil <it>Sitophilus oryzae</it> (Coleoptera), a major pest of stored cereals. The molecule responsible for toxicity was purified, by solvent extraction and HPLC, and identified as a saponin, namely 3-GlcA-28-AraRhaxyl-medicagenate. Saponins are detergents, and the CMC of this molecule was found to be 0.65 mg per mL. Neither the worm <it>Caenorhabditis elegans</it> nor the bacteria <it>E. coli</it> were found to be sensitive to this saponin, but growth of the yeast <it>Saccharomyces cerevisiae</it> was inhibited at concentrations higher than 100 μg per mL. The purified molecule is toxic for the adults of the rice weevils at concentrations down to 100 μg per g of food, but this does not apply to the others insects tested, including the coleopteran <it>Tribolium castaneum</it> and the Sf9 insect cultured cells.</p> <p>Conclusions</p> <p>This specificity for the weevil led us to investigate this saponin potential for pest control and to propose the hypothesis that this saponin has a specific mode of action, rather than acting <it>via</it> its non-specific detergent properties.</p

Growing Atmospheric Emissions of Sulfuryl Fluoride

The potent greenhouse gas sulfuryl fluoride (SO2F2) is increasingly used as a fumigant, replacing methyl bromide, whose structural and soil fumigation uses have been phased out under the Montreal Protocol. We use measurements on archived air samples and in situ observations from the Advanced Global Atmospheric Gases Experiment (AGAGE) and a box model of the global atmosphere to show a global increase of SO2F2 mole fraction from 0.3 ± 0.02 to 2.5 ± 0.08 ppt along with a global increase in emissions from 0.5 ± 0.4 Gg yr−1 to 2.9 ± 0.4 Gg yr−1 from 1978 to 2019. Based on a hybrid model incorporating bottom-up industry data and a top-down downscaling approach, we estimate the spatial distribution and trend in SO2F2 regional emissions between 2000 and 2019 and propose that the global emissions increase is driven by the growing use of SO2F2 in structural fumigation in North America and in postharvest treatment of grains and other agricultural products worldwide.publishedVersio