Results 41 to 50 of about 1,310,756 (110)
Floods of Gediz River and Disaster Management (1860-1901)
Akarsular, doğa olaylarına karşı alınan tedbirlerin çok daha kısıtlı olduğu eski zamanlarda, günümüze nispeten daha sık taşarak etraflarına önemli miktarda zararlar vermekteydiler. 19. yüzyılda sık bir şekilde taşan nehirlerden birisi de Kütahya’ya bağlı Gediz kasabasının doğusundaki dağlardan kaynağını alan ve 275 km yol aldıktan sonra Ege Denizi’ne ...
SATILMIŞ, Selahattin +1 more
openaire +2 more sources
Abstract The surface of modern Mars is largely shaped by wind, but the influence of past wind activity is less well constrained. Sedimentary rocks exposed in the lower foothills of Aeolis Mons, the central mound within Gale crater, record a transition from predominantly lacustrine deposition in the Murray formation to aeolian deposition in the Mirador ...
Amelie L. Roberts +19 more
wiley +1 more source
Abstract Climate and catchment characteristics, particularly land and water use and management, may vary according to the population growth rate, future food habits and water demands. Three climate simulations corresponding to the Intergovernmental Panel on Climate Change, Special Report on Emissions Scenarios (A1B) were downscaled using the ‘Providing
Rajesh Nune +6 more
wiley +1 more source
Stratigraphic Revision of the Selendi, Güre, and Uşak Neogene Basins, Western Anatolia
Abstract In a re‐examination of the Neogene stratigraphy of the Uşak, Güre, and Selendi basins of western Anatolia, western Turkey, the stratigraphic position of the previously defined İnay Group is revised, which was previously considered to be of the Middle Miocene age.
Fikret GÖKTAŞ +2 more
wiley +1 more source
Comparing estimates of actual evapotranspiration from satellites, hydrological models, and field data: a case study from Western Turkey [PDF]
Evapotranspiration / Estimation / Remote sensing / Satellite surveys / Field tests / Measurement / Productivity / Crops / Water requirements / Water balance / Irrigation management / River basins / Hydrology / Models / Turkey / Gediz ...
Droogers, P., Kite, G.
core
Abstract Determining the contribution of human activities to drought occurrence or aggravation of drought is an essential issue in drought risk management. Drought begins under the influence of meteorological processes and propagates to hydrological drought, which human activities affect.
Jamal Ahmadi Lavin +3 more
wiley +1 more source
Severe Impacts on Water Resources Projected for the Mediterranean Basin
Impact of climate change on water resources in the Mediterranean Basin, showing increasing (upwards arrow), decreasing (downwards arrow), and inconclusive projections (up down arrow). ABSTRACT Water resources are becoming increasingly scarce in the Mediterranean Basin due to climate change.
J. P. C. Eekhout +3 more
wiley +1 more source
Late‐Stage Aqueous Activity at Gale Crater, Mars, Recorded by Sediment Fans Eroded From Aeolis Mons
Abstract Gale crater, the landing site of NASA's Curiosity rover, and the mountain at its center, Aeolis Mons, hosts an extensive record of sedimentary rocks, which provide a window into the climate history of Mars. Curiosity has demonstrated that Gale hosted long‐lived lakes early in its history, indicating warm, quiescent surface conditions, before ...
Joel M. Davis +11 more
wiley +1 more source
The Selendi lacustrine basin developed as a supra‐detachment basin on the Simav detachment fault in response to the continental extension in western Türkiye and the associated uplift of the Menderes Massif. The facies assemblages show an aggradational stacking pattern developed throughout deposition of the basin. This stacking pattern records a balance
Ayhan Ilgar +4 more
wiley +1 more source
Sheep flock near Gediz, Hermos
A sheep flock in the village settled along Gediz River in the Agean Region. Known as Hermos in the ancient Greek or Latenized as Hermus, the Gediz River is the second-largest river in Anatolia flowing into the Aegean Sea, only second to Büyük Menderes ...
Gonnet-Bağana, Hatice
core +1 more source

