| dc.identifier.citation | Adji, Tjahyo Nugroho; Haryono, Eko; dan Woro, Suratman. (1999). Kawasan Karst dan Prospek Pengembangannya. Makalah dalam Seminar Pertemuan Ilmiah Tahunan Ikatan Geografiwan Indonesia 1999. Universitas Indonesia, 26-27 Oktober 1999. Awang, S.A. dan Nurhadi. (2005). Konservasi Sumber Air Tambakromo: Ketersediaan dan Kelangkaan Air. dalam Awang, S.A. 2005. Kelangkaan Air: Mitos Sosial, Kiat dan Ekonomi Rakyat. Yogyakarta: Debut Press. Ford, D. dan Williams, P. (1992). Karst Geomorphology and Hydrology. London: Chapman and Hall. Santosa, Langgeng Wahyu. (2007). Kerusakan Telaga Dolin dan Faktor-Faktornya di Wilayah Perbukitan Karst Kabupaten Gunungkidul. Jurnal Kebencanaan Indonesia, Vol.1(3). Hal 176-193. Sudarmadji; Suprayogi, S. dan Setiadi. (2012). Konservasi Mata Air Berbasis Masyarakat di Kabupaten Gunungkidul untuk Mengantisipasi Dampak Perubahan Iklim. Yogyakarta: Penerbit Sekolah Pascasarjana Universitas Gadjah Mada. Thornthwaite, C.W. dan J.R. Mather. (1957). Introduction and Tables for computing Potensial Evapotranspiration and The Water Balance. Publ. In Clim. Vol. 10(3). Certerton. New Jersey. Veni, G. dan DuChene, H. (2001). Living With Karst: A Fragile Foundation. Alexandria: American Geological Institute. | en_US |
| dc.description.abstract | The objective of this study is to understand the influence of meteorological conditions of logva water
availability in karst area, Gunungkidul Regency. Meteorological condition analysis was determined by
creating meteorological water balance using Thornthwaite Mather method. Water availability condition
was determined by using multi-temporal images. Then, the result of water balance was matched with the
logva water availability derived from multi-temporal images. The result shows that meteorological conditions
will influence logva water availability in karst area, Gunungkidul Regency. It was shown by comparing
the amount of logva in sur plus months and deficit months. The amount of logva in surplus
months is more than in deficit months. In addition, the longer meteorological water deficit, the amounts of
detected logva decreases. Based on that condition, it means that meteorological water balance analysis can
be used to plan disaster mitigation based on the time and duration of deficit months. | en_US |
