LEADER 03840nam 22006735 450 001 9910298380703321 005 20200706075301.0 010 $a3-319-08858-0 024 7 $a10.1007/978-3-319-08858-7 035 $a(CKB)3710000000202712 035 $a(EBL)1783138 035 $a(OCoLC)889304095 035 $a(SSID)ssj0001295598 035 $a(PQKBManifestationID)11735842 035 $a(PQKBTitleCode)TC0001295598 035 $a(PQKBWorkID)11342716 035 $a(PQKB)10251092 035 $a(MiAaPQ)EBC1783138 035 $a(DE-He213)978-3-319-08858-7 035 $a(PPN)179928007 035 $a(EXLCZ)993710000000202712 100 $a20140719d2014 u| 0 101 0 $aeng 135 $aur|n|---||||| 181 $ctxt 182 $cc 183 $acr 200 10$aSystem Engineering Applied to Fuenmayor Karst Aquifer (San Julián de Banzo, Huesca) and Collins Glacier (King George Island, Antarctica) /$fby David Chinarro 205 $a1st ed. 2014. 210 1$aCham :$cSpringer International Publishing :$cImprint: Springer,$d2014. 215 $a1 online resource (174 p.) 225 1 $aSpringer Theses, Recognizing Outstanding Ph.D. Research,$x2190-5053 300 $aDescription based upon print version of record. 311 $a3-319-08857-2 320 $aIncludes bibliographical references at the end of each chapters. 327 $aIntroduction -- Techniques -- Karst and Glacial Hydrology -- Fuenmayor Aquifer -- Collins Glacier -- Final Conclusions -- Appendices -- Glossary. 330 $aThis thesis tackles fundamental questions concerning the discharge of a pre-Pyrenean karst aquifer system and an Antarctic glacier system, utilizing a system engineering methodology and data-driven approach. It presents for the first time a simplified and effective linear transfer function for karst aquifers. The author provides detailed wavelet spectrum results, which reveal certain non-linearities in drought periods. In addition, structures based on Hammerstein-Wiener blocks have yielded a nonlinear model that is substantially more efficient than its linear counterparts. Another pioneering finding is the use of wavelet coherence between glacier discharge and air temperature to estimate SEC (Seasonal Effective Core) boundaries. The yearly SEC is essential to obtaining a model based on Hammerstein-Wiener structures, which offers considerably higher efficiency. Moreover, two different types of glacier dynamics have been discovered (overdamped and overshoot), depending on the annual cycle and the SEC average temperature. 410 0$aSpringer Theses, Recognizing Outstanding Ph.D. Research,$x2190-5053 606 $aHydrogeology 606 $aMathematical physics 606 $aStatistical physics 606 $aHydrogeology$3https://scigraph.springernature.com/ontologies/product-market-codes/G19005 606 $aMathematical Applications in the Physical Sciences$3https://scigraph.springernature.com/ontologies/product-market-codes/M13120 606 $aApplications of Nonlinear Dynamics and Chaos Theory$3https://scigraph.springernature.com/ontologies/product-market-codes/P33020 615 0$aHydrogeology. 615 0$aMathematical physics. 615 0$aStatistical physics. 615 14$aHydrogeology. 615 24$aMathematical Applications in the Physical Sciences. 615 24$aApplications of Nonlinear Dynamics and Chaos Theory. 676 $a620.001171 700 $aChinarro$b David$4aut$4http://id.loc.gov/vocabulary/relators/aut$01060008 801 0$bMiAaPQ 801 1$bMiAaPQ 801 2$bMiAaPQ 906 $aBOOK 912 $a9910298380703321 996 $aSystem Engineering Applied to Fuenmayor Karst Aquifer (San Julián de Banzo, Huesca) and Collins Glacier (King George Island, Antarctica)$92510135 997 $aUNINA