Randy Lia Weil made two highly unusual decisions about the 5millionshelefttobedonatedafterherdeath.Thefirstwasthatsheappointed14peoplesheknewandtrustedtoselecttheorganizationsandindividualswhowouldreceivefunding.Mostofthemwerelifelongactivistswithdecadesofpassionatededicationtoenvironmental,culturalandsocialjusticeissues.Thesecondunusualthingwasthatsheleftnoinstructionsforhowortowhomtheyshouldgiveherbequest.Shetrustedthemtodecide.Thiswouldprovetobeanadventureandadiscovery,andnotwithoutitschallengesfortheparticipants.EveryonesincerelywantedtobearesponsiblegrantmakeranddowhatRandywouldhavewanted.Butitwasacomplexjourneytoturnagroupofpassionateindividualsintoagroupofeffectivefunders.Beforetheycouldmakeanygrants,theyhadtoagreeontheirmission,vision,andvalues.TheyalsohadtodecidehowtheywouldoperateandmakedecisionsinawaythathonoredRandyandthevaluesthatledhertochoosethem.Itwasatallorder.AfterspendingayearplanningtoestablishtheFoundation,TheLiaFundawardedgrantsto107organizationsfrom2007to2013.Mostofthegrantsrangedfrom5,000 to 25,000.IntotaltheFoundationgaveaway5 million. This is the story of what The Lia Fund did, how they did it, and what they learned. It describes the impact of this type of grantmaking on some of the most important issues of our time. It also looks at what foundations and individual donors might learn from this adventure in philanthropy
An understanding is being developed for processes which may be important in the atmosphere, and the definition and analysis of baroclinic experiments utilizing the geophysical fluid flow cells (GFFC) apparatus in microgravity space flights. Included are studies using numerical codes, theoretical models, and terrestrial laboratory experiments. The numerical modeling is performed in three stages: calculation of steady axisymmetric flow, calculation of fastest-growing linear eigenmodes, and nonlinear effects (first, wave-mean flow interactions, then wave-wave interactions). The code can accommodate cylindrical, spherical, or channel geometry. It uses finite differences in the vertical and meridional directions, and is spectral in the azimuthal. The theoretical work was mostly in the area of effects of topography upon the baroclinic instability problem. The laboratory experiments are performed in a cylindrical annulus which has a temperture gradient imposed upon the lower surface and an approximately isothermal outer wall, with the upper and inner surfaces being nominally thermally insulating
The purpose of this study was to compare anthropometric and lower body power measurements between current professional and amateur male rugby union players. The present study also sought to determine which anthropometric and physical performance variables were predictive of playing standard. Thirty professional and 30 amateur RU players performed Wattbike 6 s maximal effort (WB6S) and countermovement (CMJ) and squat jump (SJ) assessments, anthropometric measures were also taken. Dependant variables recorded and analysed including: body mass, stature, Σ8 site skinfolds, WB6S absolute and relative peak power, CMJ and SJ average concentric force, jump height, peak velocity, time to peak force, rate of force development (RFD) and absolute and relative peak force and power. Professional players were heavier, taller and leaner than their amateur counterparts (p < 0.05). Professional players performed significantly better in all physical performance measures except CMJ and SJ time to peak force, CMJ RFD and SJ relative peak force. Variables which were predictive of playing standard were: Σ8 skinfolds, CMJ peak velocity and WB6S absolute and relative peak power (p < 0.05). These findings indicate that the current body of male professional RU players is anthropometrically and physically superior to their amateur counterparts, although not all variables assessed here were predictive of playing standard. Data presented here indicate that Σ8 skinfolds, WB6S absolute and relative power and CMJ peak velocity are predictive of playing standard, whereas other anthropometric and strength and power variables are not