HETerogeneous vectorized or Parallel (HETPv1.0): an updated inorganic heterogeneous chemistry solver for the metastable-state NH₄⁺–Na⁺–Ca<sup>2+</s... by S. J. Miller, P. A. Makar, C. J. Lee

“…These improvements include (i) the use of the “interpolate, truncate and project” (ITP) root-finding approach rather than bisection, (ii) the allowance of search interval endpoints as valid roots at the onset of a search, (iii) the use of a more accurate method to solve polynomial subsystems of equations, (iv) the elimination of negative concentrations during iterative solutions, (v) corrections for mass conservation enforcement, and (vi) several code structure improvements. …”
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Modelo matemático aplicado a la dinámica del nitrógeno en suelos manejados con praderas del sur de Chile Mathematical model applied to the dynamica of nitrogen in soils under pastu... by Paulina Alejandra Salazar Espinoza, Juan Alfredo Gómez Fernández, Pedro Antonio Núñez Ramos

“…The modified model consists of a system of partial differential equations (PDE), which consists of EDP's for N-NO and N-NO3-, while N-NH4+ was interpolated by a polynomial with the degree varying with the season. …”
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Variabilidade espacial de atributos de solos em unidades de manejo em área piloto de produção integrada de coco Soil spatial variation and properties as related to manegement units... by João Bosco Vasconcellos Gomes, Edson Luis Bolfe, Nilton Curi, Humberto Rollemberg Fontes, Antonio Carlos Barreto, Robson Dantas Viana

“…Contour maps were drawn using the kriging interpolator method. The mapped area is characterized by a broad summit of low coastal tablelands, with a closed depression in the far south of the area. …”
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Effects of intermittent generation on the economics and operation of prospective baseload power plants by Kearns, Jordan Taylor

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Effects of spatial resolution on WRF v3.8.1 simulated meteorology over the central Himalaya by J. Singh, N. Singh, N. Ojha, A. Sharma, A. Pozzer, A. Pozzer, N. Kiran Kumar, K. Rajeev, S. S. Gunthe, V. R. Kotamarthi

“…Model results show a significant improvement in d03 (<span class="inline-formula"><i>P</i></span> <span class="inline-formula">=</span> 827.6 hPa, <span class="inline-formula"><i>T</i></span> <span class="inline-formula">=</span> 19.8 <span class="inline-formula">^∘</span>C, RH <span class="inline-formula">=</span> 92.3 %), closer to the GVAX observations (<span class="inline-formula"><i>P</i></span> <span class="inline-formula">=</span> 801.4 hPa, <span class="inline-formula"><i>T</i></span> <span class="inline-formula">=</span> 19.5 <span class="inline-formula">^∘</span>C, RH <span class="inline-formula">=</span> 94.7 %). Interpolating the output from the coarser domains (d01, d02) to the altitude of the station reduces the biases in pressure and temperature; however, it suppresses the diurnal variations, highlighting the importance of well-resolved terrain (d03). …”
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Development of on-site self-calibration and retrieval methods for sky-radiometer observations of precipitable water vapor by M. Momoi, M. Momoi, R. Kudo, K. Aoki, T. Mori, K. Miura, H. Okamoto, H. Irie, Y. Shoji, A. Uchiyama, O. Ijima, M. Takano, M. Takano, T. Nakajima

“…The aerosol optical properties at the water vapor channel are interpolated from those at aerosol channels. Second, PWV is retrieved using the angular distribution of the normalized radiances at the water vapor channel. …”
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A Numerical reassessment of the Gulf of Mexico carbon system in connection with the Mississippi River and global ocean by L. Zhang, Z. G. Xue, Z. G. Xue, Z. G. Xue

“…The biogeochemical boundaries were interpolated from NCAR's CESM2-WACCM-FV2 solution after evaluating the performance of 17 GCMs in the GoM waters. …”
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SPATIOTEMPORAL CHANGES IN VELOCITY OF MELLOR GLACIER, EAST ANTARCTICA USING LANDSAT-8 DATA by P. H. Pandit, U. Khot, S. D. Jawak, S. D. Jawak, A. J. Luis

“…All the resultant velocity rasters were interpolated and bias was calculated between seasons of two consecutive years. …”
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Bilimsel Toplantı Duyuruları by Adli Tıp Uzmanları Derneği ATUD

“…Frau Schilbach Nussbaumstr.7 80336 München sschilba@psy.med.uni-muenchen.de 13th International Forensic Science Symposium 16-19 October 2001 Interpol General Secretariat, Lyon 16th Meeting of the International Association of Forensic Sciences 2-7 Sep. 2002, Société Internationale De Congres Et Services 337, rue de la Combe Caude 34090 MONTPELLIER -France Phone: + 33 (0)4 67 63 53 40 Fax: +33 (0)4 67 41 94 27 algcsi@mnet.fr www.iafs2002.com…”
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Bilimsel Toplantı Duyuruları by Adli Tıp Uzmanları Derneği ATUD

“…Frau Schilbach Nussbaumstr.7 80336 München sschilba@psy.med.uni-muenchen.de 13th International Forensic Science Symposium 16-19 October 2001 Interpol General Secretariat, Lyon 16th Meeting of the International Association of Forensic Sciences 2-7 Sep. 2002, Société Internationale De Congres Et Services 337, rue de la Combe Caude 34090 MONTPELLIER -France Phone: + 33 (0)4 67 63 53 40 Fax: +33 (0)4 67 41 94 27 algcsi@mnet.fr www.iafs2002.com…”
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Application of Variance-Distance exponential model in geochemical studies of zinc calamine ore deposit (Mehdiabad mining complex of Yazd) by Nasrin Sadrmohammadi, Seyed Reza Mehrnia, Khalil Rezaei, Selma Kadioğlu, Mahmood Honarvar

“…Consequently, a total of 180 litho-samples of Calamine region were collected and interpolated to find the anomalous populations. A GIS-based software (Spatial Analyst) was used here to obtain geometric and statistical quantities which are necessary for variance-distance equation (Teymoorian-Motlagh et al., 2012). …”
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Traitement des diagraphies acoustiques. Troisième partie : caractérisation d'un réservoir par diagraphies acoustiques obtenues avec un outil dipolaire Full-Waveform Acoustic Data... by Wicquart E., Mari J. L.

“…In these partially gas-saturated zone in the reservoir, the porosity was interpolated. The porosity log thus computed is shown in Figure 20. …”
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Spring Frost Early Warning for Apple Orchards Using WRF Model by S.M. Ebnehejazi, H. Yazdanpanah, S. Movahedi, M.A. Nasr-Esfahani, M. Moradizadeh

“…Model's hindcasts at 03:00 UTC hour for each of 51 synoptic weather stations of northwest of Iran in internal computational grid were interpolated by MATLAB software with interp 3 function using linear method, then the obtained values were compared to minimum temperature observed in the stations by using MAE, MSE, RMSE and MSSS indicators. …”
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Numerical Analysis of Natural Convection Driven Flow of a Non-Newtonian Power-Law Fluid in a Trapezoidal Enclosure with a U-Shaped Constructal by Sardar Bilal, Maryam Rehman, Samad Noeiaghdam, Hijaz Ahmad, Ali Akgül

“…To acquire information regarding the change in displacement w.r.t time and temperature, supplementary quadratic interpolating functions are also observed. An amalgam meshing is constructed to elaborate the triangular and quadrilateral elements of the trapezoidal domain. …”
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Application of a Generalized Secant Method to Nonlinear Equations with Complex Roots by Avram Sidi

“…For each integer <i>k</i>, this method generates a sequence <inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><mo>{</mo><msub><mi>x</mi><mi>n</mi></msub><mo>}</mo></mrow></semantics></math></inline-formula> of approximations to a real root of <inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><mi>f</mi><mo>(</mo><mi>x</mi><mo>)</mo></mrow></semantics></math></inline-formula>, where, for <inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><mi>n</mi><mo>≥</mo><mi>k</mi></mrow></semantics></math></inline-formula>, <inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><msub><mi>x</mi><mrow><mi>n</mi><mo>+</mo><mn>1</mn></mrow></msub><mo>=</mo><msub><mi>x</mi><mi>n</mi></msub><mo>−</mo><mi>f</mi><mrow><mo>(</mo><msub><mi>x</mi><mi>n</mi></msub><mo>)</mo></mrow><mo>/</mo><msubsup><mi>p</mi><mrow><mi>n</mi><mo>,</mo><mi>k</mi></mrow><mo>′</mo></msubsup><mrow><mo>(</mo><msub><mi>x</mi><mi>n</mi></msub><mo>)</mo></mrow></mrow></semantics></math></inline-formula>, <inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><msub><mi>p</mi><mrow><mi>n</mi><mo>,</mo><mi>k</mi></mrow></msub><mrow><mo>(</mo><mi>x</mi><mo>)</mo></mrow></mrow></semantics></math></inline-formula> being the polynomial of degree <i>k</i> that interpolates <inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><mi>f</mi><mo>(</mo><mi>x</mi><mo>)</mo></mrow></semantics></math></inline-formula> at <inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><msub><mi>x</mi><mi>n</mi></msub><mo>,</mo><msub><mi>x</mi><mrow><mi>n</mi><mo>−</mo><mn>1</mn></mrow></msub><mo>,</mo><mo>…</mo><mo>,</mo><msub><mi>x</mi><mrow><mi>n</mi><mo>−</mo><mi>k</mi></mrow></msub></mrow></semantics></math></inline-formula>, the order <inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><msub><mi>s</mi><mi>k</mi></msub></semantics></math></inline-formula> of this method satisfying <inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><mn>1</mn><mo><</mo><msub><mi>s</mi><mi>k</mi></msub><mo><</mo><mn>2</mn></mrow></semantics></math></inline-formula>. …”
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A collection of seminorms linking the <inline-formula><math display="inline"><semantics><mi mathvariant="bold-script">A</mi></semantics></math></inline-formula>-numerical radius an... by Salma Aljawi, Kais Feki, Zakaria Taki

“…This seminorm is defined using a continuous increasing and bijective function <inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><mi>f</mi><mo>:</mo><msup><mi mathvariant="double-struck">R</mi><mo>+</mo></msup><mo>⟶</mo><msup><mi mathvariant="double-struck">R</mi><mo>+</mo></msup></mrow></semantics></math></inline-formula> and an interpolational path <inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><msub><mi mathvariant="fraktur">m</mi><mi>λ</mi></msub></semantics></math></inline-formula> of the symmetric mean <inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mi mathvariant="fraktur">m</mi></semantics></math></inline-formula>. …”
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Airborne observations during KORUS-AQ show that aerosol optical depths are more spatially self-consistent than aerosol intensive properties by S. E. LeBlanc, S. E. LeBlanc, M. Segal-Rozenhaimer, M. Segal-Rozenhaimer, M. Segal-Rozenhaimer, J. Redemann, C. Flynn, R. R. Johnson, S. E. Dunagan, R. Dahlgren, R. Dahlgren, J. Kim, M. Choi, M. Choi, M. Choi, A. da Silva, P. Castellanos, Q. Tan, Q. Tan, L. Ziemba, K. Lee Thornhill, K. Lee Thornhill, M. Kacenelenbogen

“…</p> <p>Understanding the variability of aerosols helps reduce uncertainties in the aerosol direct radiative effect by quantifying the errors due to interpolating between sparse aerosol observation sites or modeled pixels, potentially reducing uncertainties in the upcoming observational capabilities. …”
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Dergilerden Özetler by Osman Eren Karpuzoğlu

“…Bulunabilen dental ve tıbbi kayıtları içeren antemor- tem bilgiler, INTERPOL’ün felaket kurbanı kimliklendirme formlarına geçirildi. …”
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Dergilerden Özetler by Osman Eren Karpuzoğlu

“…Bulunabilen dental ve tıbbi kayıtları içeren antemor- tem bilgiler, INTERPOL’ün felaket kurbanı kimliklendirme formlarına geçirildi. …”
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Time-dependent source apportionment of submicron organic aerosol for a rural site in an alpine valley using a rolling positive matrix factorisation (PMF) window by G. Chen, Y. Sosedova, Y. Sosedova, F. Canonaco, F. Canonaco, R. Fröhlich, A. Tobler, A. Tobler, A. Vlachou, K. R. Daellenbach, C. Bozzetti, C. Hueglin, P. Graf, U. Baltensperger, J. G. Slowik, I. El Haddad, A. S. H. Prévôt

“…However, since the contribution of this factor was insignificant (2.1 %), we did not attempt to interpolate its potential source in this work. The uncertainties (<span class="inline-formula"><i>σ</i></span>) for the modelled OA factors (i.e. rotational uncertainty and statistical variability in the sources) varied from <span class="inline-formula">±</span>4 % (58-OA) to a maximum of <span class="inline-formula">±</span>40 % (LO-OOA). …”
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