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Books on the topic 'MLT circulation'

Author: Grafiati

Published: 6 September 2023

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1

Yun, Sŏng-bŏm. Haeyang isang hyŏnsang kamsi pangan mit yech'ŭk yŏn'gu. Inch'ŏn-si: Kukt'o Haeyangbu Kungnip Haeyang Chosawŏn, 2011.

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2

Ding, Yulong. Fundamental studies on the production of high carbon ferrochromium using melt circulation. Birmingham: University of Birmingham, 1997.

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3

Kouker, Wolfgang. Eine Studie zur Klimatologie der mittleren Atmosphäre mit Hilfe eines 3-D Zirkulationsmodells. Berlin: D. Reimer, 1988.

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4

Langematz, Ulrike. Eine dreidimensionale Modellsimulation der Zirkulation in der Mittleren Atmosphäre mit Aspekten troposphärisch-stratosphärischer Wechselwirkungen: (DK 551.506.7/551.510.53 ... Berlin: D. Reimer, 1991.

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5

Chŏng, Hyŏn-t'ae. Konggong tosŏgwan taech'ul yŏnch'e pangji mit hoesuyul hyangsang pangan yŏn'gu: Tosŏgwan Yŏn'guso 2009-yŏndo hyŏmnyŏk yŏn'gu, 2. Sŏul T'ŭkpyŏlsi: Tosŏgwan Yŏn'guso, 2009.

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6

Görgen, Klaus. Sensitivitätsstudien und Analyse von Atmosphäre-Meereis-Wechselwirkungen mit dem regionalen Atmosphärenmodell HIRHAM4 auf Basis eines neu entwickelten beobachtungsgestützten unteren Modellantriebs während ausgewählter Sommer über der Arktis, Laptewsee: Sensitivity studies and analysis of atmosphere-sea-ice-interactions with the regional atmospheric model HIRHAM4 using a newly developed observational lower boundary forcing dataset during selected summers over the Arctic/Laptev Sea. Bremen: Alfred-Wegener-Institut für Polar- und Meeresforschung, 2006.

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7

Holger, Fischer. Vergleichende Untersuchungen eines optimierten dynamisch-thermodynamischen Meereismodells mit Beobachtungen im Weddellmeer =: Comparison of an optimized dynamic-thermodynamic sea ice model with observations in the Weddell Sea. Bremerhaven: Alfred-Wegener-Institut für Polar- und Meeresforschung, 1995.

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8

Fieg, Kerstin. Der Ozean als Teil des gekoppelten Klimasystems: Versuch der Rekonstruktion der glazialen Zirkulation mit verschieden komplexen Atmosphärenkomponenten = The ocean as a part of the coupled climate system : an attempt to reconstruct the glacial circulation with different models of the atmosphere. Bremerhaven: Alfred-Wegener-Institut für Polar- und Meeresforschung, 1996.

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9

Weber, Anne-Katrin. Television before TV. Nieuwe Prinsengracht 89 1018 VR Amsterdam Nederland: Amsterdam University Press, 2022. http://dx.doi.org/10.5117/9789463727815.

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Television before TV rethinks the history of interwar television by exploring the medium’s numerous demonstrations organized at national fairs and international exhibitions in the late 1920s and 1930s. Building upon extensive archival research in Britain, Germany, and the United States, Anne-Katrin Weber analyses the sites where the new medium met its first audiences. She argues that public displays were central to television’s social construction; for the historian, the exhibitions therefore constitute crucial events to understand not only the medium’s pre-war emergence, but also its subsequent domestication in the post-war years. Designed as a transnational study, her book highlights the multiple circulations of artefacts and ideas across borders of democratic and totalitarian regimes alike. Richly illustrated with 100 photographs, Weber finally emphasizes that even without regular programmes, interwar television was widely seen.

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10

Kay, Hailbronner, Klein Eckart Dr, and Kokott Juliane, eds. Einwanderungskontrolle und Menschenrechte =: Immigration control and human rights : Beiträge anlässlich des Symposiums am 29./30. Juni 1998 in Potsdam, finanziert mit Unterstützung des German Marshall Fund der Vereinigten Staaten von Amerika und des Menschenrechtszentrums an der Universität Potsdam. Heidelberg: C.F. Müller, 1999.

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11

Beyer, J., and K. Messmer. Organdurchblutung und Sauerstoffversorgung Bei PEEP: Tierexperimentelle Untersuchungen Zur Regionalen Organdurchblutung und Lokalen Sauerstoffversorgung Bei Beatmung Mit Positiv-Endexspiratorischem Druck. Springer London, Limited, 2013.

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12

Yang, Kun. Observed Regional Climate Change in Tibet over the Last Decades. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.587.

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The Tibetan Plateau (TP) is subjected to strong interactions among the atmosphere, hydrosphere, cryosphere, and biosphere. The Plateau exerts huge thermal forcing on the mid-troposphere over the mid-latitude of the Northern Hemisphere during spring and summer. This region also contains the headwaters of major rivers in Asia and provides a large portion of the water resources used for economic activities in adjacent regions. Since the beginning of the 1980s, the TP has undergone evident climate changes, with overall surface air warming and moistening, solar dimming, and decrease in wind speed. Surface warming, which depends on elevation and its horizontal pattern (warming in most of the TP but cooling in the westernmost TP), was consistent with glacial changes. Accompanying the warming was air moistening, with a sudden increase in precipitable water in 1998. Both triggered more deep clouds, which resulted in solar dimming. Surface wind speed declined from the 1970s and started to recover in 2002, as a result of atmospheric circulation adjustment caused by the differential surface warming between Asian high latitudes and low latitudes.The climate changes over the TP have changed energy and water cycles and has thus reshaped the local environment. Thermal forcing over the TP has weakened. The warming and decrease in wind speed lowered the Bowen ratio and has led to less surface sensible heating. Atmospheric radiative cooling has been enhanced, mainly through outgoing longwave emission from the warming planetary system and slightly enhanced solar radiation reflection. The trend in both energy terms has contributed to the weakening of thermal forcing over the Plateau. The water cycle has been significantly altered by the climate changes. The monsoon-impacted region (i.e., the southern and eastern regions of the TP) has received less precipitation, more evaporation, less soil moisture and less runoff, which has resulted in the general shrinkage of lakes and pools in this region, although glacier melt has increased. The region dominated by westerlies (i.e., central, northern and western regions of the TP) received more precipitation, more evaporation, more soil moisture and more runoff, which together with more glacier melt resulted in the general expansion of lakes in this region. The overall wetting in the TP is due to both the warmer and moister conditions at the surface, which increased convective available potential energy and may eventually depend on decadal variability of atmospheric circulations such as Atlantic Multi-decadal Oscillation and an intensified Siberian High. The drying process in the southern region is perhaps related to the expansion of Hadley circulation. All these processes have not been well understood.

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13

Webb, Andrew. Colloids in critical illness. Oxford University Press, 2016. http://dx.doi.org/10.1093/med/9780199600830.003.0056.

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Colloid solutions are homogenous mixtures of large molecules suspended in a crystalloid solution. The efficacy of colloids as volume substitutes or expanders, and length of effect are determined by their physicochemical properties. Smaller volumes of colloid than crystalloid are required for resuscitation. The primary use of colloids is in the correction of circulating volume. Rather than using fixed haemodynamic endpoints, fluid can be given in small aliquots with assessment of the dynamic haemodynamic response to each aliquot. The aim of a fluid challenge is to produce a small, but significant (200 mL) and rapid increase in plasma volume with changes in central venous pressure or stroke volume used to judge fluid responsiveness. Colloid fluids give a reliable increase in plasma volume to judge fluid responsiveness.

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14

Secăreanu, George. Dezvoltarea inteligenta a ariilor rurale profund dezavantajate din Romania. Editura Universitara, 2022. http://dx.doi.org/10.5682/9786062814199.

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Cartea prezinta si dezbate situatia ariilor rurale profund dezavantajate de la nivelul Romaniei, precum si dezvoltarea inteligenta a acestora. Ca sa facem o mica paranteza, ea nu se adreseaza doar spatiului romanesc, intrucat propune metode de surprindere si de tratament pentru ariile subdezvoltate. Astfel, ea prezinta doua perspective: cea in care sunt determinate acele arii rurale profund dezavantajate si cea de-a doua parte, care cuprinde modul in care ariile respective pot fi dezvoltate. Complexitatea problematicii spatiului rural reprezinta o tema in care geografii o au sub observatie, identificand tipuri de probleme cu care acestia se confrunta. Odata cu progresul tehnologic si cu circulatia fluxurilor de informatii la care are acces cu precadere populatia din mediul urban, spatiul rural incepe sa prezinte un dezinteres pentru actorii ce ar putea sa le mentina. Spun sa le mentina, intrucat trendul la nivel global este acela ca, preponderent, locuitorii sa ii regasim in mediul urban. Desigur, in aceasta conjunctura decalajale tind sa creasca si mai mult intre administratii si, implicit, intre nivelul de trai din aceeasi societate.

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15

Soar, Jasmeet, and Jerry P. Nolan. Artificial ventilation in cardiopulmonary resuscitation. Oxford University Press, 2016. http://dx.doi.org/10.1093/med/9780199600830.003.0060.

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When cardiac arrest occurs, cardiopulmonary resuscitation (CPR) should be started with chest compressions first. The use of ventilations is determined by the training of rescuers, their ability and willingness to provide rescue breaths, patient characteristics, and the underlying cause of the cardiac arrest. Trained rescuers should give two ventilations after every 30 compressions, or once the airway is secured with a tracheal tube, ventilate the patient at 10 breaths/min without any pause in chest compressions. Rescuers who are unable or unwilling to provide effective ventilation, while awaiting expert help should use compression-only CPR. Ventilations are needed for the treatment of cardiac arrest in children, when arrest is from a primary respiratory cause, or during a prolonged cardiac arrest. Choice of ventilation technique depends on rescuer skills and the airway used. Effective oxygenation and ventilation can be maintained during CPR with a tidal volume of approximately 500 mL given over an inspiratory time of 1 second. Rescuers should give supplemental oxygen in as high a concentration as possible during CPR in order to rapidly correct tissue hypoxia. Once restoration of a spontaneous circulation has been achieved the inspired oxygen should be adjusted to maintain oxygen saturation between 94 and 98%.

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