The Relationship between the IC₅₀ Values and the Apparent Inhibition Constant in the Study of Inhibitors of Tyrosinase Diphenolase Activity Helps Confirm the Mechanism o... by Pablo Garcia-Molina, Francisco Garcia-Molina, Jose Antonio Teruel-Puche, Jose Neptuno Rodriguez-Lopez, Francisco Garcia-Canovas, Jose Luis Muñoz-Muñoz

“…The non-linear regression adjustment of <inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><msub><mi>i</mi><mi mathvariant="normal">D</mi></msub></mrow></semantics></math></inline-formula> with respect to the initial inhibitor concentration <inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><msub><mrow><mrow><mo>[</mo><mi mathvariant="normal">I</mi><mo>]</mo></mrow></mrow><mn>0</mn></msub></mrow></semantics></math></inline-formula> allows for the calculation of the inhibitor concentration necessary to inhibit the activity by 50%, at a given substrate concentration (IC₅₀), thus avoiding making interpolations between different values of <inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><msub><mi>i</mi><mi mathvariant="normal">D</mi></msub></mrow></semantics></math></inline-formula>. …”
Get full text

Firn data compilation reveals widespread decrease of firn air content in western Greenland by B. Vandecrux, B. Vandecrux, M. MacFerrin, H. Machguth, H. Machguth, W. T. Colgan, D. van As, A. Heilig, C. M. Stevens, C. Charalampidis, R. S. Fausto, E. M. Morris, E. Mosley-Thompson, L. Koenig, L. N. Montgomery, C. Miège, S. B. Simonsen, T. Ingeman-Nielsen, J. E. Box

“…We quantify FAC in both the uppermost 10&thinsp;m and the entire firn column before interpolating FAC over the entire ice-sheet firn area as an empirical function of long-term mean air temperature (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mover accent="true"><mrow><msub><mi>T</mi><mtext>a</mtext></msub></mrow><mo mathvariant="normal">‾</mo></mover></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="12pt" height="16pt" class="svg-formula" dspmath="mathimg" md5hash="3f34f2e28fd131f1588d0a4a19d8cca4"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-13-845-2019-ie00001.svg" width="12pt" height="16pt" src="tc-13-845-2019-ie00001.png"/></svg:svg></span></span>) and net snow accumulation (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M2" display="inline" overflow="scroll" dspmath="mathml"><mrow><mover accent="true"><mover accent="true"><mi>c</mi><mo mathvariant="normal">˙</mo></mover><mo mathvariant="normal">‾</mo></mover><mo>)</mo></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="12pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="2467b5ce9e85c5b99553be3356b76c30"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-13-845-2019-ie00002.svg" width="12pt" height="15pt" src="tc-13-845-2019-ie00002.png"/></svg:svg></span></span>. …”
Get full text

GRAVITY ANOMALIES OF THE CRUST AND UPPER MANTLE FOR CENTRAL AND SOUTH ASIA by V. N. Senachin, A. A. Baranov

“…For the surrounding regions, data on the structure and properties of the crust were taken from the CRUST 2.0 model [Bassin et al., 2000] and interpolated to the 1´1° grid. Thus, data with the resolution of 1´1° were used to describe the sediments and the crust, and data with the resolution of 0.1´0.1° characterized the water layer (batimetry).Model GGM01 based on satellite observation data of the GRACE project (http://www.csr.utexas.edu) simulated the Earth's gravity field and was used to calculate anomalies in ‘free’ air across the entire surface of our model, which took into account the correction for the elevation of an observation object. …”
Get full text

Validation of GRASP algorithm product from POLDER/PARASOL data and assessment of multi-angular polarimetry potential for aerosol monitoring by C. Chen, C. Chen, O. Dubovik, D. Fuertes, P. Litvinov, T. Lapyonok, A. Lopatin, F. Ducos, Y. Derimian, M. Herman, D. Tanré, L. A. Remer, A. Lyapustin, A. M. Sayer, A. M. Sayer, R. C. Levy, N. C. Hsu, J. Descloitres, L. Li, L. Li, B. Torres, Y. Karol, M. Herrera, M. Herreras, M. Aspetsberger, M. Wanzenboeck, L. Bindreiter, D. Marth, A. Hangler, C. Federspiel

“…The subjects of the validation are spectral aerosol optical depth (AOD), aerosol absorption optical depth (AAOD) and single-scattering albedo (SSA) at six wavelengths, as well as Ångström exponent (AE), fine-mode AOD (AODF) and coarse-mode AOD (AODC)<span id="page3574"/> interpolated to the reference wavelength 550 nm. Second, an inter-comparison of PARASOL/GRASP products with the PARASOL/Operational, MODIS Dark Target (DT), Deep Blue (DB) and Multi-Angle Implementation of Atmospheric Correction (MAIAC) aerosol products for the year 2008 was performed. …”
Get full text

Information processing in short-term memory tasks by Monsell, S, Stephen Monsell

“…Further experiments are suggested to compare the effects in the various short-term memory tasks of semantic similarity, rate of presentation, and interpolated material. In conclusion it is suggested that a greater emphasis on the representation of motor as well as perceptual events does much tc clarify the nature of active memory.…”

Mary I. Ingraham, Joseph K. So, and Roy Moodley, eds. 2016. Opera in a Multicultural World: Coloniality, Culture, Performance. New York: Routledge by Jane Forner

“…This is evident especially in the longer printed version of the libretto, in which images from historical and modern archives are interpolated amid the text (Clarke, 1999). Conceiving of these operas as representing a mode of articulating difference on stage that is temporally and geographically specific, the authors examine the works in tandem with issues of production and performance. …”
Get full text