PPT-A Level-Set Method for Multimaterial Radiative Shock Hydrod

MULTIMAT 2011 September 59 Arcachon France David Starinshak and Smadar Karni Department of Mathematics University of Michigan Center for Radiative Shock Hydrodynamics CRASH Funding DoE NNSAASC grant DEFC5208NA28616 NSF Award DMS . R adiative - , Page 1 Radiative and Radiative - Convecti ve Equilibrium Introduction The energy balance of the Earth’ ytem i quite intricate with numerou Experimental . Astrophysics Research. Department of Atmospheric. Oceanic & Space Sciences. Applied Physics . Program. Department of Physics. Michigan Institute for Plasma Science and Engineering. Astrophysical and Laboratory Plasmas. Lecture 1: Temperature-Density regime. . Many physical processes. . Focus on . Atomic+Plasma. interactions. . Atomic properties are . intrinsic. , . independent of external factors (temp, den, etc.). tropical cyclones. Robert Fovell and . Yizhe. Peggy Bu. University of California, Los Angeles. rfovell@ucla.edu. 1. Thanks to. : . Greg . Thompson, NCAR/. DTC; Ligia . Bernardet. and Mrinal . Biswas. Corrections. Peter Schnatz. Stony Brook University. Radiative. Events. In scattering experiments, a photon may be emitted by a charged particle due to . Bremsstrahlung. radiation.. This type of radiation is due to the deceleration of a charged particle as it approaches the . In astronomy, the main source of information about celestial bodies and other objects is the visible light or more generally electromagnetic radiation.. From Wikipedia.. It also is important for the atmosphere of Earth, so you’ll meet it if you are going into Earth atmosphere science…. the . Radiative Effects . of . Black Carbon Internal Mixing. Charles Li. Group Meeting Presentation. October 1, 2014. Group Meeting 10/1/14. 1. Black Carbon (BC) Direct Radiative Forcing:. +0.71 W m. Hydrodynamics. Fall 2011 Review. Experimental data from CRASH experiments. Carolyn Kuranz. CRASH experiments have produced data from shock breakout to 30 ns. Shock Breakout data (~450 . ps. ). Diagnostics. imbalance . 1985-2012. Richard P. Allan. , . Chunlei. . Liu (University of Reading/NCAS Climate); Norman Loeb (NASA Langley); Matt Palmer (Met Office). r.p.allan@reading.ac.uk. @. rpallanuk. GEWEX 7. Feedbacks. . “Our understanding of the climate system is complicated by . feedbacks. that either . amplify. or . damp. perturbations…”. Feedbacks. . Describe the inter-related growth or decay of the components of a system.. of. aerosols over clouds . and. clear skies determined using CALIPSO . and. the A-Train. Robert Wood. , . Duli. . Chand. , Tad Anderson. University of Washington. VOCALS RF04, 21 November 2008. Effect of aerosol layer on TOA SW radiation. Shock. Decreased tissue perfusion . . inadequate O2 delivery . . . tiessue. ischemia. Common Clinical Features of Shock. 1. HYPOTENSION. SBP < 90 mm Hg. MAP <60 mm Hg. Acute decreased in SBP of > 40 mm Hg. . Overview of Model: Convection. . The convection scheme of . Emanuel and . Živkovic. -Rothman. . (1999) . uses a buoyancy sorting algorithm . and . represents an entire spectrum of convective clouds, from shallow, non-precipitating cumulus to deep precipitating cumulonimbus. Precipitation re-evaporates and drives an unsaturated downdraft that imports enthalpy and moisture into the subcloud layer. Re-evaporation of cloud water, resulting from entrainment of dry air, drives penetrative downdrafts within the clouds. The cloud base mass flux is continuously relaxed so as to produce near neutrality of a parcel lifted dry adiabatically, and then moist adiabatically, to the first level above its lifted condensation level. This maintains a form of boundary layer . Kerry Emanuel. Massachusetts Institute of Technology. Several Possibly Inter-related Enigmas of the Tropical Atmosphere. Why does moist convection often cluster?. What determines the number of tropical cyclones on the planet?.