Contribution of expanded marine sulfur chemistry to the seasonal variability of dimethyl sulfide oxidation products and size-resolved sulfate aerosol by L. Tashmim, W. C. Porter, Q. Chen, B. Alexander, C. H. Fite, C. D. Holmes, J. R. Pierce, B. Croft, S. Ishino

“…We find that this updated mechanism collectively decreases the global mean surface-layer gas-phase sulfur dioxide (<span class="inline-formula">SO₂</span>) mixing ratio by 40 % and enhances the sulfate aerosol (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M3" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msubsup><mi mathvariant="normal">SO</mi><mn mathvariant="normal">4</mn><mrow><mn mathvariant="normal">2</mn><mo>-</mo></mrow></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="29pt" height="17pt" class="svg-formula" dspmath="mathimg" md5hash="6060a0eb6022af681aa55d19b3180df9"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-24-3379-2024-ie00001.svg" width="29pt" height="17pt" src="acp-24-3379-2024-ie00001.png"/></svg:svg></span></span>) mixing ratio by 17 %. …”
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Biomass burning CO, PM and fuel consumption per unit burned area estimates derived across Africa using geostationary SEVIRI fire radiative power and Sentinel-5P CO data by H. M. Nguyen, H. M. Nguyen, J. He, J. He, M. J. Wooster, M. J. Wooster, M. J. Wooster

“…The use of satellite-based CO observations to derive biome-specific CO emission coefficients, <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mrow><msubsup><mi mathvariant="normal">EC</mi><mi mathvariant="normal">CO</mi><mi mathvariant="normal">b</mi></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="29pt" height="17pt" class="svg-formula" dspmath="mathimg" md5hash="3b24a326bb052d8d5cd8496cce50b733"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-23-2089-2023-ie00001.svg" width="29pt" height="17pt" src="acp-23-2089-2023-ie00001.png"/></svg:svg></span></span>, addresses key uncertainties in the use of AOD observations to estimate fire-generated CO emissions including the requirement for a smoke mass extinction coefficient in the AOD to TPM conversion and the large variation in TPM emission factors – which are used to convert TPM emissions to CO emissions. …”
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Regional carbon fluxes from land use and land cover change in Asia, 1980–2009 by Leonardo Calle, Josep G Canadell, Prabir Patra, Philippe Ciais, Kazuhito Ichii, Hanqin Tian, Masayuki Kondo, Shilong Piao, Almut Arneth, Anna B Harper, Akihiko Ito, Etsushi Kato, Charlie Koven, Stephen Sitch, Benjamin D Stocker, Nicolas Vivoy, Andy Wiltshire, Sönke Zaehle, Benjamin Poulter

“…The estimates are aggregated spatially to Southeast, East, and South Asia and temporally for three decades, 1980–1989, 1990–1999 and 2000–2009. Since 1980, net carbon emissions from LULCC in Asia were responsible for 20%–40% of global LULCC emissions, with emissions from Southeast Asia alone accounting for 15%–25% of global LULCC emissions during the same period. …”
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Microbial diversity of drilling fluids from 3000&thinsp;m deep Koyna pilot borehole provides insights into the deep biosphere of continental earth crust by H. Bose, A. Dutta, A. Roy, A. Gupta, S. Mukhopadhyay, B. Mohapatra, J. Sarkar, S. Roy, S. K. Kazy, P. Sar

“…Change of pH to alkalinity, reduced abundance of Si and Al, but enrichment of Fe, Ca and <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msubsup><mi mathvariant="normal">SO</mi><mn mathvariant="normal">4</mn><mrow><mn mathvariant="normal">2</mn><mo>-</mo></mrow></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="29pt" height="17pt" class="svg-formula" dspmath="mathimg" md5hash="43c7521f547bc9d1c731092871dcc89b"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="sd-27-1-2020-ie00001.svg" width="29pt" height="17pt" src="sd-27-1-2020-ie00001.png"/></svg:svg></span></span> in the samples from deeper horizons suggested a gradual infusion of elements or ions from the crystalline bedrock, leading to an observed geochemical shift in the DF. …”
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Reactive interaction between migmatite-related melt and mafic rocks: clues from the Variscan lower crust of Palmi (southwestern Calabria, Italy) by M. R. Renna

“…</p> <p>Both whole-rock and amphibole analyses reveal a decrease in Mg# (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M10" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><mi mathvariant="normal">Mg</mi><mo>/</mo><mo>(</mo><mi mathvariant="normal">Mg</mi><mo>+</mo><msup><mi mathvariant="normal">Fe</mi><mrow><mn mathvariant="normal">2</mn><mo>+</mo></mrow></msup><mo>)</mo></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="80pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="53b83642251cf5f4808a9a15e1f66258"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-35-1-2023-ie00001.svg" width="80pt" height="15pt" src="ejm-35-1-2023-ie00001.png"/></svg:svg></span></span>) from amphibolite layers within paragneiss to fine- and medium-grained rocks of the main body. …”
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Measurement report: Atmospheric CH₄ at regional stations of the Korea Meteorological Administration–Global Atmosphere Watch Programme: measurement, characteristics, and... by H. Lee, H. Lee, W. Seo, S. Li, S. Lee, S. T. Kenea, S. Joo

“…<p>To quantify <span class="inline-formula">CH₄</span> emissions at policy-relevant spatial scales, the Korea Meteorological Administration (KMA) started monitoring its atmospheric levels in 1999 at Anmyeondo (AMY) and expanded monitoring to Jeju Gosan Suwolbong (JGS) and Ulleungdo (ULD) in 2012. …”
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Eksistensi Kedaulatan Negara dalam Penerapan Yurisdiksi Mahkamah Pidana Internasional by Danel Aditia Situngkir

“…Bandung: Kini Media Bhakti Ardhiwisastra, Yudha. 1999. Imunitas Kedaulatan Negara di Forum Pengadilan Negeri Asing. …”
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Improved ozone monitoring by ground-based FTIR spectrometry by O. E. García, E. Sanromá, E. Sanromá, M. Schneider, F. Hase, S. F. León-Luis, S. F. León-Luis, T. Blumenstock, E. Sepúlveda, A. Redondas, V. Carreño, C. Torres, N. Prats

“…The present paper examines the performance of different O<span class="inline-formula">₃</span> retrieval strategies from FTIR (Fourier transform infrared) spectrometry by using the 20-year time series of the high-resolution solar spectra acquired from 1999 to 2018 at the subtropical Izaña Observatory (IZO, Spain) within NDACC (Network for the Detection of Atmospheric Composition Change). …”
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Elevated Factor VIII and von Willebrand Factor Levels Predict Unfavorable Outcome in Stroke Patients Treated with Intravenous Thrombolysis by Noémi Klára Tóth, Edina Gabriella Székely, Katalin Réka Czuriga-Kovács, Ferenc Sarkady, Orsolya Nagy, Levente István Lánczi, Ervin Berényi, Klára Fekete, István Fekete, László Csiba, László Csiba, Zsuzsa Bagoly, Zsuzsa Bagoly

“…Long-term functional outcome was determined at 90 days after the event by the modified Rankin scale (mRS).ResultsVWF levels on admission were significantly elevated in case of more severe AIS [median and IQR values: NIHSS &lt;6:189.6% (151.9–233.2%); NIHSS 6–16: 199.6% (176.4–250.8%); NIHSS &gt;16: 247.8% (199.9–353.8%), p = 0.013]; similar, but non-significant trend was observed for FVIII levels. …”
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Nine years of warming and nitrogen addition in the Tibetan grassland promoted loss of soil organic carbon but did not alter the bulk change in chemical structure by H. Sun, H. Sun, M. W. I. Schmidt, J. Li, J. Li, X. Liu, N. O. E. Ofiti, S. Zhou, M. Nie

“…Here we used a 9-year two-way factorial experiment involving warming with open top chambers (<span class="inline-formula">+</span>1.80 <span class="inline-formula">^∘C</span> in the daytime and <span class="inline-formula">+</span>0.77 <span class="inline-formula">^∘C</span> in the nighttime at the soil surface) and multilevel nitrogen (N) enrichment treatments (0, 5, 10, and 15 <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M6" display="inline" overflow="scroll" dspmath="mathml"><mrow class="unit"><mi mathvariant="normal">g</mi><mspace width="0.125em" linebreak="nobreak"/><msup><mi mathvariant="normal">m</mi><mrow><mo>-</mo><mn mathvariant="normal">2</mn></mrow></msup><mspace linebreak="nobreak" width="0.125em"/><msup><mi mathvariant="normal">yr</mi><mrow><mo>-</mo><mn mathvariant="normal">1</mn></mrow></msup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="50pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="dc81c6a4cfb4aab0a71631113845e6e0"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-21-575-2024-ie00001.svg" width="50pt" height="15pt" src="bg-21-575-2024-ie00001.png"/></svg:svg></span></span>) in the TP to investigate the changes in soil organic carbon (SOC) pool size and chemical structure. …”
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Peculiarities of the development of oral speech for foreign students by Olga Zlotnyk-Shagina

“…E-mail: ozlotnik@bigmir.net   REFERENCES • Bippus, A., Daly J. (1999). What Do People Think Causes Stage Fright?: Naïve Attributions about the Reasons for Public Speaking Anxiety. …”
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Statistical distribution of mirror-mode-like structures in the magnetosheaths of unmagnetized planets – Part 2: Venus as observed by the Venus Express spacecraft by M. Volwerk, C. Simon Wedlund, D. Mautner, S. Rojas Mata, G. Stenberg Wieser, Y. Futaana, C. Mazelle, D. Rojas-Castillo, C. Bertucci, M. Delva

“…The ratios of the observations during solar minimum and maximum are slightly dependent on the depth <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mrow><mi mathvariant="normal">Δ</mi><mi>B</mi><mo>/</mo><mi>B</mi></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="32pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="d63ce14a50f80a491be31c20befafcd4"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="angeo-41-389-2023-ie00001.svg" width="32pt" height="14pt" src="angeo-41-389-2023-ie00001.png"/></svg:svg></span></span> of the structures; deeper structures are more prevalent at solar maximum. …”
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Influence of CO₂ adsorption on cylinders and fractionation of CO₂ and air during the preparation of a standard mixture by N. Aoki, S. Ishidoya, S. Murayama, N. Matsumoto

“…The CO<span class="inline-formula">₂</span> molar fractions in the standard mixtures deviated from the gravimetric values by <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M8" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>-</mo><mn mathvariant="normal">0.207</mn><mo>±</mo><mn mathvariant="normal">0.060</mn></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="76pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="3418d786b3358a1d2a69404f3c186384"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="amt-15-5969-2022-ie00001.svg" width="76pt" height="10pt" src="amt-15-5969-2022-ie00001.png"/></svg:svg></span></span> <span class="inline-formula">µmol mol⁻¹</span> on average, which is larger than the compatibility goal (0.1 <span class="inline-formula">µmol mol⁻¹</span>) recommended by the World Meteorological Organization. …”
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Ensemble analysis and forecast of ecosystem indicators in the North Atlantic using ocean colour observations and prior statistics from a stochastic NEMO–PISCES simulator by M. Popov, J.-M. Brankart, A. Capet, A. Capet, E. Cosme, P. Brasseur

“…An example application is provided, which covers a limited time period in a limited subregion of the North Atlantic (between 31 and 21<span class="inline-formula">^∘</span> W, between 44 and 50.5<span class="inline-formula">^∘</span> N, between 15 March and 15 June 2019, at a <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M3" display="inline" overflow="scroll" dspmath="mathml"><mrow><mn mathvariant="normal">1</mn><mo>/</mo><mn mathvariant="normal">4</mn></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="20pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="b5e3e9140aa7b06ea772efeaf94fa8b6"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="os-20-155-2024-ie00001.svg" width="20pt" height="14pt" src="os-20-155-2024-ie00001.png"/></svg:svg></span></span><span class="inline-formula">^∘</span> and a 1 d resolution). …”
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Culicidae (Diptera: Culicomorpha) in the southern Brazilian ‘Ana Leuch Lozovei’ collection, with notes on distribution and diversity by Maurício dos Santos Conceição, Samira Chahad-Ehlers, Luiz Gonzaga dos Santos-Neto, Adson Luís Sant’Ana, Gabriela Princival Marques Ribeiro, Débora do Rocio Klisiowicz, Cássio Lázaro Silva-Inacio, Taciano de Moura Barbosa, Renata Antonaci Gama, Ana Leuch Lozovei, Andrey José de Andrade

“…Culicids were collected using different methodologies in 18 municipalities in Paraná state, between 1967 and 1999. There are 5,739 catalogued specimens, of which 4,703 (81.94%) are identified at species level, with a diversity of 100 species. …”
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Artigo 04: A ATUAÇÃO DO ADVOGADO NA ÁREA DE DIREITO DESPORTIVO: A LEGISLAÇÃO COMO FONTE FORMAL DE "RUPTURA" by Dr. Alberto dos Santos Puga Barbosa

“…Rio de Janeiro: Forense/Gryphus, 1999. MELO FILHO, A. Direito Desportivo Atual. Rio de Janeiro: Forense, 1986. …”
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Characteristics of Silicone Oil Emulsification After Vitrectomy for Rhegmatogenous Retinal Detachment: An Ultrasound Biomicroscopy Study by Hongmei Zhao, Hongmei Zhao, Hongmei Zhao, Hongmei Zhao, Hongmei Zhao, Jian Yu, Jian Yu, Jian Yu, Jian Yu, Jian Yu, Yuan Zong, Yuan Zong, Yuan Zong, Yuan Zong, Yuan Zong, Chunhui Jiang, Chunhui Jiang, Chunhui Jiang, Chunhui Jiang, Chunhui Jiang, Haohao Zhu, Gezhi Xu, Gezhi Xu, Gezhi Xu, Gezhi Xu, Gezhi Xu

“…The mean total SO emulsification grade was 19.99 ± 12.98 (range: 1–36). Younger age and male (both P &lt; 0.05) were associated with higher total SO emulsification grade. …”
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An ensemble of 48 physically perturbed model estimates of the 1∕8° terrestrial water budget over the conterminous United States, 1980–2015 by H. Zheng, W. Fei, W. Fei, Z.-L. Yang, J. Wei, J. Wei, L. Zhao, L. Zhao, L. Li, L. Li, S. Wang

“…</p> <p>The dataset spans from 1980 to 2015 over the conterminous United States (CONUS) at a monthly temporal resolution and a <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M3" display="inline" overflow="scroll" dspmath="mathml"><mrow><mn mathvariant="normal">1</mn><mo>/</mo><mn mathvariant="normal">8</mn></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="20pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="cae1aad9ff7f755b0d46b5c0a78adc1e"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="essd-15-2755-2023-ie00003.svg" width="20pt" height="14pt" src="essd-15-2755-2023-ie00003.png"/></svg:svg></span></span><span class="inline-formula">^∘</span> spatial resolution. …”
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Temporal evolution of temperatures in the Red Sea and the Gulf of Aden based on in situ observations (1958–2017) by M. Agulles, G. Jordà, G. Jordà, B. Jones, S. Agustí, C. M. Duarte, C. M. Duarte

“…Regarding long-term evolution, our results show only positive trends above 40&thinsp;m depth, with maximum trends of 0.045&thinsp;<span class="inline-formula">+</span>&thinsp;0.016&thinsp;<span class="inline-formula">^∘</span>C&thinsp;decade<span class="inline-formula">⁻¹</span> at 15&thinsp;m, and the largest negative trends at 125&thinsp;m (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M5" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>-</mo><mn mathvariant="normal">0.072</mn><mo>+</mo><mn mathvariant="normal">0.011</mn></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="76pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="48c55c72dddecbc845c6722f85d0a768"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="os-16-149-2020-ie00001.svg" width="76pt" height="10pt" src="os-16-149-2020-ie00001.png"/></svg:svg></span></span>&thinsp;<span class="inline-formula">^∘</span>C&thinsp;decade<span class="inline-formula">⁻¹</span>). …”
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Effect of Fe–Fe interactions and <i>X</i>-site vacancy ordering on the OH-stretching spectrum of foitite by E. Balan, G. Radtke, C. Fourdrin, L. Paulatto, H. A. Horn, Y. Fuchs

“…Based on the theoretical results, the two bands at 3630 and 3644 cm<span class="inline-formula">⁻¹</span> in the vibrational spectra of iron-rich and Na-deficient tourmalines are assigned to <span class="inline-formula">^<i>W</i></span>OH groups associated with <span class="inline-formula">^<i>Y</i></span>Fe<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M13" display="inline" overflow="scroll" dspmath="mathml"><mrow><msubsup><mi/><mn mathvariant="normal">2</mn><mrow><mn mathvariant="normal">2</mn><mo>+</mo></mrow></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="12pt" height="16pt" class="svg-formula" dspmath="mathimg" md5hash="8a0e45b5f456bbd3c431526c1d0d38cf"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-35-105-2023-ie00001.svg" width="12pt" height="16pt" src="ejm-35-105-2023-ie00001.png"/></svg:svg></span></span><span class="inline-formula">^<i>Y</i></span>Al<span class="inline-formula">³⁺</span> environments with an AFM coupling of Fe ions and surrounded by one and two vacant <span class="inline-formula"><i>X</i></span> sites, respectively. …”
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