01047nam a2200265 i 4500991001651389707536060530s1995 enk b 001 0 eng d0198289774b13405834-39ule_instDip.to Studi Giuridiciita338.7 Penrose, Edith Tilton128544The theory of the growth of the firm /Edith Penrose ; with a new foreword by the author3rd ed.Oxford ;New York :Oxford University Press,1995xxiii, 272 p. ;23 cmContiene riferimenti bibliografici e indiceOrganizzazione industrialeTeoria economicaImpreseSviluppoTeoria economica .b1340583421-09-0630-05-06991001651389707536LE027 338.70 PEN01.0112027000121724le027-E40.20-l- 00000.i1424315530-05-06Theory of the Growth of the Firm433451UNISALENTOle02730-05-06ma -engenk4005145nam 2201597z- 450 991055736610332120220111(CKB)5400000000042230(oapen)https://directory.doabooks.org/handle/20.500.12854/76745(oapen)doab76745(EXLCZ)99540000000004223020202201d2021 |y 0engurmn|---annantxtrdacontentcrdamediacrrdacarrierMultiscale Impacts of Anthropogenic and Climate Changes on Tropical and Mediterranean HydrologyBasel, SwitzerlandMDPI - Multidisciplinary Digital Publishing Institute20211 online resource (372 p.)3-0365-1236-5 3-0365-1237-3 The atmospheric part of the water cycle is accelerating, affecting hydrological dynamics, especially in tropical and Mediterranean areas, where landscapes, soils and territories are particularly vulnerable to global warming and land use changes. Across four continents and a dozen of different regions or basins, this SI strives to highlight the environmental and societal vulnerabilities and their links with the water cycle. The basins of three of the greatest basins in the world in terms of streamflows-the Amazon River, the Orinoco River and the Congo River-show their unexpected behaviors. This book aims to present past and present status to improve future land and water management.Research & information: generalbicsscAfricaagroforestryAmazonbank gulliesbasementbifurcationBouregregbroom grassCameroonCasiquiarecatchment hydrologyclimate changeCongo River Basincritical droughtdamdata preprocessingdatabasedepletion (or recession) coefficientdischarge forecastDoDdonor selectiondrainage area ratiodroughtENSEMBLEerosionEuphrates basinextreme rainfall eventsflow recession modelFouta Djallonfrequency analysisFula societyGambia Riverhumid tropicshydro-sedimentary budgethydroclimatic variableshydroclimatologyhydrogeochemicalhydrological modelinghydrosedimentologyimpact assessmentimpervious areainter-rill erosioninverse distance weightedinverse estuarieslakelakeshoresland managementland-cover changeLiDARM3C2mangroveMediterranean regionmodelingMono basinMontane Southeast Asiamonthly gridsMoroccomoving averageMUSLEn/aNiger RiverOrinocooverland flowphysical similarityprecipitation deficitrainfallrainfall shiftRambla de Algecirasregional climate modelsrubberrunoffrunoff coefficientsandstonesemi-aridSenegal RiverSenegal River BasinSeyhan River basinsiltingsoil erosionsoil water holding capacitysolid transportSouth-East Asiaspatial drought analysisstandardized precipitation index (SPI)streamflowstreamflow estimationteak tree plantationtrend detectiontrendsUAVunderstoryungauged basinsurbanizationwater balancewater salinitywater towerWest AfricaResearch & information: generalDescroix Lucedt704357Mahé GiledtLaraque AlainedtRibolzi OlivieredtLacombe GuillaumeedtDescroix LucothMahé GilothLaraque AlainothRibolzi OlivierothLacombe GuillaumeothBOOK9910557366103321Multiscale Impacts of Anthropogenic and Climate Changes on Tropical and Mediterranean Hydrology3030619UNINA