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Journal articles on the topic "W 85 h43498 2008"
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Kiecana, Irena, Elżbieta Mielniczuk, Małgorzata Cegiełko, and Aleksandra Szołkowska. "Grzyby porażające korzenie i podstawę źdźbła owsa (Avena sativa L.)." Biuletyn Instytutu Hodowli i Aklimatyzacji Roślin, no. 247 (March 31, 2008): 73–79. http://dx.doi.org/10.37317/biul-2008-0074.
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Badania przeprowadzono w latach 2004–006 na polach Hodowli Roślin Danko w Kopaszewie, woj. wielkopolskie. W każdym sezonie wegetacji w fazie dojrzałości późno-woskowej ziarna (87 w skali Tottmana (1987) oceniano porażenie korzeni i dolnych międzywęźli źdźbeł. Odsetek źdźbeł wykazujących objawy chorobowe wynosił od 32 (Rajtar) do 85% (Deresz) w 2004 roku, od 44 (Gniady) do 93% (Breton) w 2005 roku i od 8 (Cwał) do 34.5% (Rajtar) w 2006 roku. Średnio po 3 latach badań udział źdźbeł z objawami nekrozy korzeni i podstawy źdźbeł wynosił od 42% w przypadku odmiany Rajtar do 64 w przypadku odmiany Breton. Analiza mikologiczna chorych roślin wykazała, że przyczyną chorób podsuszkowych owsa, w każdym sezonie wegetacji były grzyby z rodzaju Fusarium, a w szczególności gatunek F. culmorum oraz Bipolaris sorokiniana.
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Jarecki, Wacław, and Dorota Bobrecka-Jamro. "Reakcja pszenicy jarej odmiany Parabola na dolistne dokarmianie mocznikiem i Mikrokomplexem." Biuletyn Instytutu Hodowli i Aklimatyzacji Roślin, no. 262 (December 29, 2011): 39–46. http://dx.doi.org/10.37317/biul-2011-0003.
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W latach 2008–2010 przeprowadzono ścisłe doświadczenie polowe, którego celem było określenie reakcji roślin pszenicy jarej na dolistne dokarmianie. Stwierdzono, że zastosowane nawozy: mocznik, Mikrokomplex oraz mieszanka mocznika z Mikrokomplexem nie zmodyfikowały istotnie liczby ziaren w kłosie i MTN, jednak plon nasion na obiektach dokarmianych był większy w porównaniu do obiektu kontrolnego, przy czym istotna różnica dotyczyła tylko łącznej aplikacji mocznika z Mikrokomplexem. Wyrównanie i celność ziarna wyniosły średnio 85% i nie zostały istotnie zróżnicowane przez badany czynnik. Największą zawartość białka ogólnego oznaczono w ziarnie pozyskanym z obiektów dokarmianych azotem i wyniosła ona 14,6%.
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LEPIARCZYK, ANDRZEJ, TEOFIL ŁABZA, and KATARZYNA PUŻYŃSKA. "Produkcyjność pszenicy ozimej odmiany Turnia i Rysa wysiewanej w siewie czystym i mieszanym w zależności od systemu uprawy roli." Agronomy Science 65, no. 3 (October 28, 2010): 43–50. http://dx.doi.org/10.24326/as.2010.3.5.
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Badania prowadzono w ścisłym doświadczeniu płodozmianowym założonym w Stacji Doświadczalnej Katedry Agrotechniki i Ekologii Rolniczej Uniwersytetu Rolniczego w Krakowie-Mydlnikach (50˚08' N, 19˚85' E). Doświadczenie polowe realizowano w latach 2006–2008 metodą losowanych bloków w czterech powtórzeniach. Przedplonem pszenicy ozimej był bobik. Pierwszym czynnikiem doświadczenia był system uprawy roli (płużny – tradycyjny i bezpłużny – uproszczony). Drugim czynnikiem doświadczenia była odmiana pszenicy ozimej (Turnia i Rysa) wysiewana w siewie czystym lub mieszanym (w stosunku 1:1). Oceny produkcyjności odmian pszenicy ozimej w zależności od zróżnicowanej uprawy roli dokonano w oparciu o plon ziarna, białka ogólnego i wartości energetycznej plonu, przyjmując, że 1 kg s.m. = 18,41 MJ. Stwierdzono istotne zróżnicowanie produkcyjności odmian wyrażonej plonem suchej masy, białka ogólnego i energii.
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Bolibok, Piotr. "Zadłużenie gospodarstw domowych a dynamika wydatków konsumpcyjnych w krajach OECD po wybuchu kryzysu finansowego." Kwartalnik Kolegium Ekonomiczno-Społecznego. Studia i Prace, no. 1 (November 23, 2017): 145–58. http://dx.doi.org/10.33119/kkessip.2017.1.9.
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The paper aims at empirical evaluation of the impact of household debt on the dynamics of consumption spending since the beginning of the global financial crisis. The research employed linear regression analysis of the rate of growth of household spending against the rate of growth of disposable income, the level of indebtedness and long-term interest rates in the OECD member states between 2008-2014. The results obtained indicate that household indebtedness was one of the factors influencing the dynamics of consumption demand and thus the processes of economic growth in the OECD states after the beginning of the global financial crisis. Variations in the relation of total debt to net disposable income and in the level of long-term interest rates were both negatively related to the changes in consumption spending. This impact turned out to be markedly stronger when total household debt of a given country was exceeding 85% of GDP, which is consistent with the results of previous investigations on the in&uence of the indebtedness of household sector on the dynamics of economic growth
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Bazilio, Sérgio, Zelinda Schemczssen, and Anésio Da Cunha Marques. "Registro visual do lobo-guará, Chrysocyon brachyurus (Illiger, 1815) (Mammalia: Carnivora: Canidae) na Floresta Nacional de Três Barras, SC." Biotemas 22, no. 4 (May 12, 2011): 133. http://dx.doi.org/10.5007/2175-7925.2009v22n4p133.
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http://dx.doi.org/10.5007/2175-7925.2009v22n4p133 O lobo-guará é o maior representante da família dos canídeos na América do Sul, vive em ambientes abertos, como campo e cerrado, também encontrado prόximo a brejos e matas ao longo de cursos de água. Esta nota relata a visualização direta de um exemplar na Floresta Nacional (Flona) do Ibama em Três Barras, SC (lat. 26º10'15"S; long. 50º10'15"W e elev. 750m) que é caracterizada por remanescentes de Floresta Ombrofila Mista e apresenta grandes áreas com reflorestamento de Pinus e araucária com mais de 50 anos. Possui uma área de 4.458,5 ha, isotermas de 20 a 22C em janeiro e de 12 a 14C em julho, com média de umidade relativa do ar anual de 85% e precipitações entre 1.200 e 1.400mm por ano. Um exemplar adulto foi visualizado, pela manhã, várias vezes por funcionários do Ibama no final de junho de 2008 entre as coordenadas (lat. 26º12'56"S; long. 50º18'17"W e lat. 26º12'33"S; long. 50º18'20"W). O indivíduo foi fotografado pela primeira vez em três de julho às 7h30min e a segunda vez no dia 19 do mesmo mês às 7h48min no mesmo local, na estrada de acesso à sede da Flona.
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Verkhoglyadova, O. P., B. T. Tsurutani, A. J. Mannucci, M. G. Mlynczak, L. A. Hunt, and T. Runge. "Variability of ionospheric TEC during solar and geomagnetic minima (2008 and 2009): external high speed stream drivers." Annales Geophysicae 31, no. 2 (February 19, 2013): 263–76. http://dx.doi.org/10.5194/angeo-31-263-2013.
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Abstract. We study solar wind–ionosphere coupling through the late declining phase/solar minimum and geomagnetic minimum phases during the last solar cycle (SC23) – 2008 and 2009. This interval was characterized by sequences of high-speed solar wind streams (HSSs). The concomitant geomagnetic response was moderate geomagnetic storms and high-intensity, long-duration continuous auroral activity (HILDCAA) events. The JPL Global Ionospheric Map (GIM) software and the GPS total electron content (TEC) database were used to calculate the vertical TEC (VTEC) and estimate daily averaged values in separate latitude and local time ranges. Our results show distinct low- and mid-latitude VTEC responses to HSSs during this interval, with the low-latitude daytime daily averaged values increasing by up to 33 TECU (annual average of ~20 TECU) near local noon (12:00 to 14:00 LT) in 2008. In 2009 during the minimum geomagnetic activity (MGA) interval, the response to HSSs was a maximum of ~30 TECU increases with a slightly lower average value than in 2008. There was a weak nighttime ionospheric response to the HSSs. A well-studied solar cycle declining phase interval, 10–22 October 2003, was analyzed for comparative purposes, with daytime low-latitude VTEC peak values of up to ~58 TECU (event average of ~55 TECU). The ionospheric VTEC changes during 2008–2009 were similar but ~60% less intense on average. There is an evidence of correlations of filtered daily averaged VTEC data with Ap index and solar wind speed. We use the infrared NO and CO2 emission data obtained with SABER on TIMED as a proxy for the radiation balance of the thermosphere. It is shown that infrared emissions increase during HSS events possibly due to increased energy input into the auroral region associated with HILDCAAs. The 2008–2009 HSS intervals were ~85% less intense than the 2003 early declining phase event, with annual averages of daily infrared NO emission power of ~ 3.3 × 1010 W and 2.7 × 1010 W in 2008 and 2009, respectively. The roles of disturbance dynamos caused by high-latitude winds (due to particle precipitation and Joule heating in the auroral zones) and of prompt penetrating electric fields (PPEFs) in the solar wind–ionosphere coupling during these intervals are discussed. A correlation between geoeffective interplanetary electric field components and HSS intervals is shown. Both PPEF and disturbance dynamo mechanisms could play important roles in solar wind–ionosphere coupling during prolonged (up to days) external driving within HILDCAA intervals.
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Painemal, D., and P. Zuidema. "Microphysical variability in southeast Pacific Stratocumulus clouds: synoptic conditions and radiative response." Atmospheric Chemistry and Physics 10, no. 13 (July 9, 2010): 6255–69. http://dx.doi.org/10.5194/acp-10-6255-2010.
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Abstract. Synoptic and satellite-derived cloud property variations for the southeast Pacific stratocumulus region associated with changes in coastal satellite-derived cloud droplet number concentrations (Nd) are explored. MAX and MIN Nd composites are defined by the top and bottom terciles of daily area-mean Nd values over the Arica Bight, the region with the largest mean oceanic Nd, for the five October months of 2001, 2005, 2006, 2007 and 2008. The ability of the satellite retrievals to capture composite differences is assessed with ship-based data. Nd and ship-based accumulation mode aerosol concentrations (Na) correlate well (r = 0.65), with a best-fit aerosol activation value dln Nddln Na of 0.56 for pixels with Nd>50 cm−3. The adiabatically-derived MODIS cloud depths also correlate well with the ship-based cloud depths (r=0.7), though are consistently higher (mean bias of almost 60 m). The MAX-Nd composite is characterized by a weaker subtropical anticyclone and weaker winds both at the surface and the lower free troposphere than the MIN-Nd composite. The MAX-Nd composite clouds over the Arica Bight are thinner than the MIN-Nd composite clouds, have lower cloud tops, lower near-coastal cloud albedos, and occur below warmer and drier free tropospheres (as deduced from radiosondes and NCEP Reanalysis). CloudSat radar reflectivities indicate little near-coastal precipitation. The co-occurrence of more boundary-layer aerosol/higher Nd within a more stable atmosphere suggests a boundary layer source for the aerosol, rather than the free troposphere. The MAX-Nd composite cloud thinning extends offshore to 80° W, with lower cloud top heights out to 95° W. At 85° W, the top-of-atmosphere shortwave fluxes are significantly higher (~50%) for the MAX-Nd composite, with thicker, lower clouds and higher cloud fractions than for the MIN-Nd composite. The change in Nd at this location is small (though positive), suggesting that the MAX-MIN Nd composite differences in radiative properties primarily reflects synoptic changes. Circulation anomalies and a one-point spatial correlation map reveal a weakening of the 850 hPa southerly winds decreases the free tropospheric cold temperature advection. The resulting increase in the static stability along 85° W is highly correlated to the increased cloud fraction, despite accompanying weaker free tropospheric subsidence.
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Mébarki, Y., V. Catoire, G. Berthet, N. Huret, and C. Robert. "More evidence for very short-lived substance contribution to stratospheric chlorine inferred from HCl balloon-borne in situ measurements in the tropics." Atmospheric Chemistry and Physics Discussions 9, no. 4 (July 29, 2009): 16163–95. http://dx.doi.org/10.5194/acpd-9-16163-2009.
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Abstract. Volume mixing ratio (vmr) vertical profiles of hydrogen chloride (HCl) are retrieved from in situ measurements performed by a balloon-borne infrared tunable diode laser absorption spectrometer (SPIRALE) during two balloon flights in the tropics (Teresina, Brazil, 5.1° S–42.9° W) at three year interval in June 2005 and June 2008. HCl vertical profiles obtained from 15.0 to 31.0 km are presented and analysed to estimate the contribution of very short-lived substances (VSLS) to total stratospheric chlorine. Both retrieved vertical profiles of HCl from these flights globally agree very well with each other, with estimated overall uncertainties of 6% on vmr between 23 and 31 km. Upper limits of HCl vmr as low as (20±20) pptv in June 2008 and (30±30) pptv in June 2005 are inferred in the upper part of the tropical tropopause layer (TTL). Backward trajectory calculations suggest that these low amounts were sampled in air masses corresponding to typical background conditions, i.e. neither influenced by recent tropospheric nor stratospheric air. Taking into account the recently reported VSLS source gas measurements obtained in similar conditions (Laube et al., 2008) and the main intermediate product gas (COCl2), a VSLS contribution of about (85±35 pptv) to total stratospheric chlorine is inferred. This refines the WMO (2007) estimation of 50 to 100 pptv, which was not taking into account any HCl contribution. In addition, comparisons of HCl measurements between SPIRALE and MLS-Aura satellite instrument in the tropical lower and middle stratosphere lead to a very good agreement. Since HCl modelled values derived from a total stratospheric chlorine budget including 100 pptv of VSLS agree with MLS measurements in the upper stratosphere, the consistency between SPIRALE and MLS measurements provides another evidence for this VSLS contribution.
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Mébarki, Y., V. Catoire, N. Huret, G. Berthet, C. Robert, and G. Poulet. "More evidence for very short-lived substance contribution to stratospheric chlorine inferred from HCl balloon-borne in situ measurements in the tropics." Atmospheric Chemistry and Physics 10, no. 2 (January 18, 2010): 397–409. http://dx.doi.org/10.5194/acp-10-397-2010.
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Abstract. Volume mixing ratio (vmr) vertical profiles of hydrogen chloride (HCl) are retrieved from in situ measurements performed by a balloon-borne infrared tunable diode laser absorption spectrometer (SPIRALE) during two balloon flights in the tropics (Teresina, Brazil, 5.1° S–42.9° W) in June 2005 and June 2008. HCl vertical profiles obtained from 15 to 31 km are presented and analysed to estimate the contribution of very short-lived substances (VSLS) to total stratospheric chlorine. Both retrieved vertical profiles of HCl from these flights agree very well with each other, with estimated overall uncertainties of 6% on vmr between 23 and 31 km. Upper limits of HCl vmr as low as 20 pptv in June 2008 and 30 pptv in June 2005 are inferred in the upper part of the tropical tropopause layer (TTL). Backward trajectory calculations and such low amounts suggest that the air masses sampled correspond to typical background conditions, i.e. neither influenced by recent tropospheric nor stratospheric air. Taking into account the recently reported VSL source gas measurements obtained in similar conditions (Laube et al., 2008) and the main intermediate degradation product gas COCl2 (Fu et al., 2007), a total VSLS contribution of 85±40 pptv to stratospheric chlorine is inferred. This refines the WMO (2007) estimation of 50 to 100 pptv, which was not taking into account any HCl contribution. In addition, comparisons of HCl measurements between SPIRALE and the Aura MLS satellite instrument in the tropical lower and middle stratosphere lead to a very good agreement. The previous agreement between MLS-deduced upper stratospheric total chlorine content and modelled values including 100 pptv of VSLS (Froidevaux et al., 2006) is thus supported by our present result about the VSLS contribution.
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Berenguer, Marc, Madalina Surcel, Isztar Zawadzki, Ming Xue, and Fanyou Kong. "The Diurnal Cycle of Precipitation from Continental Radar Mosaics and Numerical Weather Prediction Models. Part II: Intercomparison among Numerical Models and with Nowcasting." Monthly Weather Review 140, no. 8 (August 1, 2012): 2689–705. http://dx.doi.org/10.1175/mwr-d-11-00181.1.
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Abstract This second part of a two-paper series compares deterministic precipitation forecasts from the Storm-Scale Ensemble Forecast System (4-km grid) run during the 2008 NOAA Hazardous Weather Testbed (HWT) Spring Experiment, and from the Canadian Global Environmental Multiscale (GEM) model (15 km), in terms of their ability to reproduce the average diurnal cycle of precipitation during spring 2008. Moreover, radar-based nowcasts generated with the McGill Algorithm for Precipitation Nowcasting Using Semi-Lagrangian Extrapolation (MAPLE) are analyzed to quantify the portion of the diurnal cycle explained by the motion of precipitation systems, and to evaluate the potential of the NWP models for very short-term forecasting. The observed diurnal cycle of precipitation during spring 2008 is characterized by the dominance of the 24-h harmonic, which shifts with longitude, consistent with precipitation traveling across the continent. Time–longitude diagrams show that the analyzed NWP models partially reproduce this signal, but show more variability in the timing of initiation in the zonal motion of the precipitation systems than observed from radar. Traditional skill scores show that the radar data assimilation is the main reason for differences in model performance, while the analyzed models that do not assimilate radar observations have very similar skill. The analysis of MAPLE forecasts confirms that the motion of precipitation systems is responsible for the dominance of the 24-h harmonic in the longitudinal range 103°–85°W, where 8-h MAPLE forecasts initialized at 0100, 0900, and 1700 UTC successfully reproduce the eastward motion of rainfall systems. Also, on average, MAPLE outperforms radar data assimilating models for the 3–4 h after initialization, and nonradar data assimilating models for up to 5 h after initialization.
Books on the topic "W 85 h43498 2008"
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Health Risk and Vulnerability. Routledge, 2007.
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Wilkinson, Iain. Health, Risk and Vulnerability. Taylor & Francis Group, 2007.
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Wilkinson, Iain. Health, Risk and Vulnerability. Taylor & Francis Group, 2007.
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Wilkinson, Iain. Health, Risk and Vulnerability. Taylor & Francis Group, 2007.
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Wilkinson, Iain. Health, Risk and Vulnerability. Routledge, 2007.
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Patient Advocacy for Healthcare Quality: Strategies for Achieving Patient Centered Care. Jones & Bartlett Publishers, 2007.
Find full textConference papers on the topic "W 85 h43498 2008"
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LeBlanc, S. A., Y. Gao, and K. E. Goodson. "Thermoelectric Heat Recovery From a Tankless Water Heating System." In ASME 2008 International Mechanical Engineering Congress and Exposition. ASMEDC, 2008. http://dx.doi.org/10.1115/imece2008-68860.
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Thermoelectric cogeneration promises to recover waste heat energy from a variety of combustion systems. There is a need for computationally efficient simulations of practical systems that allow optimization and illustrate the impact of key material and system parameters. Previous research investigated thermoelectric material enhancement and thermoelectric system integration separately. This work connects material parameters and system integration. We develop a thermal simulation for a 15kW tankless, methane-fueled water heater with thermoelectric modules embedded within a cross-flow heat exchanger. The simulation employs a finite volume method for the two fluids. It links external convection with a surface efficiency of 85%, internal convection for laminar flow, and conduction through the system in order to determine power generation within the thermoelectric. For a single pipe in the water heater system, 126 W of electrical power can be generated, and a typical system could yield 370 W. Realization of effective cogeneration systems hinges on investigating the impact of thermoelectric material parameters coupled with system parameters, so the impact of varying flow rate, convection coefficient, TEM thermal conductivity, Seebeck coefficient, and thermal interface materials are investigated. While varying parameters can improve thermoelectric output by over 50%, thermal interface materials can severely limit cogeneration system power output.