01015nam 2200349 450 991016507840332120230808205335.01-5040-3064-8(CKB)4330000000012176(MiAaPQ)EBC4557176(EXLCZ)99433000000001217620160708d2016 uy| 0engurcnu||||||||rdacontentrdamediardacarrierRagtime a musical and cultural history /Edward BerlinNew York :Open Road Distribution,2016.1 online resource (197 pages) illustrations1-5040-2981-X Includes bibliographical references.Ragtime musicHistory and criticismRagtime musicHistory and criticism.Berlin Edward1378279MiAaPQMiAaPQMiAaPQBOOK9910165078403321Ragtime3416527UNINA01851oam 2200445zu 450 991101890880332120210807004642.01-118-66567-8(CKB)3450000000004548(SSID)ssj0000815199(PQKBManifestationID)11428298(PQKBTitleCode)TC0000815199(PQKBWorkID)10805969(PQKB)11568833(NjHacI)993450000000004548(PPN)189033983(EXLCZ)99345000000000454820160829d2002 uy engur|||||||||||txtccrCalibration of Watershed Models[Place of publication not identified]American Geophysical Union20021 online resource (462 pages)Bibliographic Level Mode of Issuance: Monograph0-87590-355-X During the past four decades, computer-based mathematical models of watershed hydrology have been widely used for a variety of applications including hydrologic forecasting, hydrologic design, and water resources management. These models are based on general mathematical descriptions of the watershed processes that transform natural forcing (e.g., rainfall over the landscape) into response (e.g., runoff in the rivers). The user of a watershed hydrology model must specify the model parameters before the model is able to properly simulate the watershed behavior.WatershedsMathematical modelsWatershedsMathematical models.551.48Duan Qingyun868446Sorooshian SorooshGupta Hoshin VPQKBBOOK9911018908803321Calibration of Watershed Models1938592UNINA