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ZAMAN, İKLİM VE AKARSU GELİŞİMİ

Year 2005, Volume: 3 Issue: 2, 70 - 80, 01.08.2005
https://doi.org/10.1501/Cogbil_0000000058

Abstract

Akarsu gelişimi uzun vadede (glasyal/interglasyal salınımlar) iklim değişimlerinin genel yapısına ayak uydurur. Ancak, bir soğuk-sıcak dönem ölçeğinde, akarsu aktivitesinin jeomorfolojik etkisi en iyi iklim değişiminin süresiyle açığa vurulur. Bu periyotlardaki flüvyal aktivite sadece kısa bir zaman için devam eder. Yani, bir iklim değişikliğinden sonra bir drenaj havzasındaki içsel gelişim, morfolojinin ve sedimantasyon tipinin gecikmeli tepki vermesiyle son bulur. Sonuçta, en kısa zaman ölçeğinde, yerel eşikler akarsu sisteminin vereceği tepkide oldukça belirleyici bir rol oynayabilirler. Bu çalışmada, flüvyal gelişim ile iklim arasındaki ilişkinin basit olmadığı; fakat temel olarak zamana bağlı olduğu sonucuna varılmıştır

References

  • Baulig, H. (1950) Essais de Géomorphologie, Paris, Publ. de la Faculté des Lettres de l’Université de Strasbourg, Faz. 114
  • Bohncke, S., Kasse, C. and Vandenberghe, J. (1995) “Climate induced environmental changes during the Vistulian Lateglacial at Zabinko, Poland”, Quaestiones Geographicae, Spec. Issue 4, 43 – 64.
  • Büdel, J. (1977) Klima – Geomorphologie, Gebrüder Borntrager.
  • Davis, W. M. (1899) “The geographical cycle”, Geographical Journal, 14, 481 – 504.
  • Isarin, R. (1995) “Reconstruction of the climate in Northwestern and central Europe during the Weichselian Lateglacial”, Terra Nostra, 2/95, INQUA XIV Int. Congress, Abstracts, 121.
  • Kasse, C., Vandenberghe, J. And Bohncke, S. (1995) “Climatic Change and Fluvial Dynamics of the Maas During the Late Weichselian and Eearly Holocene”, Palaoklimaforschung, 14, (in press).
  • Knox, J. (1972) “Valley Alluviation in Southwestern Wisconsin”, Annals of the Association of American Geographers, 62, 401– 410.
  • Kozarski, S. (1983) “River Channel Adjustment to Climatic Change in West Central Poland”, In: Gregory, K. (ed), Background to Palaeohydrology, 355 – 374.
  • Penck, W. (1924) Die Morphologische Analyse, Ein Kapittel der physikalischen Geologie.
  • Rose, J., Turner, C., Coope, G. R. and Bryan M. D. (1980) “Channel Changes in a Lowland River Catchment Over the Last 13,000 Years”., In: Cullingford, R. A., Davidson, D. A. and Lewin, J. (eds), Timescales in Geomorphology, 159 – 175.
  • Rose, J. and Boardman, J. (1983) “River Activity in Relation to Short – Term Climatic Deterioration”, Quaternary Studies in Poland, 4, 189 – 198.
  • Rose, J. (1995) “Lateglacial and Early Holocene River Activity in Lowland Britain”, Palaoklimaforschung, 14, (in press).
  • Ruegg, G. (1993) “Alluvial Architecture of the Quaternary Rhine – Meuse River System in the Netherland”, Geologie en Mijnbouw, 72, 321- 330.
  • Schumm, S. (1979) “Geomorphic Thresholds: The Concept and its Applications”, Transcations Institute British Geographers, 4, 485 – 515.
  • Soergel, W. (1939) “Das Diluviale System”, Fortschritte Geologie und Paleontologie, XII – 9, 1 – 92.
  • Vandenberghe, J. (1995) “Postglacial River Activity and Climate: State-Of-The-Art And Future Prospects”, Palaoklimaforschung, 14, (in press).
  • Vandenberghe, J. and Van Huissteden, J. (1988) “Fluvio – Aeolian İnteraction in a Region of Continous Permafrost”, Proceedings of the 5th International Conference on Permafrost, 1, 876 – 881.
  • Vandenberghe, J., Mommersteeg, H. and Edelman, D. (1993) “Lithogenesis And Geomorphological Processes of the Pleistocene Deposites At Maastricht – Belvedere”, Mededelingen Rijks Geologische Dienst, 47, 7 – 17.
  • Vandenberghe, J., Kasse, C., Bohncke, S. and Kozarski, S. (1994) “Climate – Related River Activity at the Weichselian – Holocene Transition: A Comparative Study of the Warta and Maas Rivers”, Terra Nova, 6, 476 – 485.
  • Van Geel, B., Coope, R. G. and Van Der Hammen, T. (1989) “Palaeoecology and Stratigraphy of the Lateglacial Type Section at Usselo (The Netherlands)”, Reviews of Palaeobotany and Palynology, 31, 359 – 448.
  • Van Huissteden, J. and Vandenberghe, J. (1988) “Changing Fluvial Style of Periglacial Lowland Rivers During the Weichselian Pleniglacial in the Eastern Netherlands”, Zeitschrift für Geomorphologie, Supplement Band, 71, 131 – 146.
  • Van Kolfschoten, T., Roebroeks, W. and Vandenberghe, J. (1993) “The Middle and Late Pleistocene Sequence at Maastricht – Belvedere: The Type Locality of the Belvedere Interglacial”, Mededelingen Rijks Geologische Dienst, 47, 81 – 91.
  • Veldkamp, A. and Kroonenberg, S. (1993) “Late Quaternary Chronology of the Allier Terrace Sediments (Masif Central, France)”, Geologie en Mijnbouw, 72, 179 – 192.

Timescales, Climate and River Development

Year 2005, Volume: 3 Issue: 2, 70 - 80, 01.08.2005
https://doi.org/10.1501/Cogbil_0000000058

Abstract

In the long term (glacial/interglacial sequences), river development follows general climatic evolution. However, at the scale of one cold-warm cycle, it appears that the geomorphological effect of river activity is best expressed at times of climatic change. Such periods of pronounced fluvial action last only a short time. In more detail, the internal evolution in a drainage basin after a climatic event results in a delayed response of the morphology and sedimentation pattern. Finally, on the shortest timescale local thresholds may play a decisive role in the reactions of river systems. It is concluded that the relation between fluvial development and climate is not a simple one, but is fundamentally dependant on the timescale

References

  • Baulig, H. (1950) Essais de Géomorphologie, Paris, Publ. de la Faculté des Lettres de l’Université de Strasbourg, Faz. 114
  • Bohncke, S., Kasse, C. and Vandenberghe, J. (1995) “Climate induced environmental changes during the Vistulian Lateglacial at Zabinko, Poland”, Quaestiones Geographicae, Spec. Issue 4, 43 – 64.
  • Büdel, J. (1977) Klima – Geomorphologie, Gebrüder Borntrager.
  • Davis, W. M. (1899) “The geographical cycle”, Geographical Journal, 14, 481 – 504.
  • Isarin, R. (1995) “Reconstruction of the climate in Northwestern and central Europe during the Weichselian Lateglacial”, Terra Nostra, 2/95, INQUA XIV Int. Congress, Abstracts, 121.
  • Kasse, C., Vandenberghe, J. And Bohncke, S. (1995) “Climatic Change and Fluvial Dynamics of the Maas During the Late Weichselian and Eearly Holocene”, Palaoklimaforschung, 14, (in press).
  • Knox, J. (1972) “Valley Alluviation in Southwestern Wisconsin”, Annals of the Association of American Geographers, 62, 401– 410.
  • Kozarski, S. (1983) “River Channel Adjustment to Climatic Change in West Central Poland”, In: Gregory, K. (ed), Background to Palaeohydrology, 355 – 374.
  • Penck, W. (1924) Die Morphologische Analyse, Ein Kapittel der physikalischen Geologie.
  • Rose, J., Turner, C., Coope, G. R. and Bryan M. D. (1980) “Channel Changes in a Lowland River Catchment Over the Last 13,000 Years”., In: Cullingford, R. A., Davidson, D. A. and Lewin, J. (eds), Timescales in Geomorphology, 159 – 175.
  • Rose, J. and Boardman, J. (1983) “River Activity in Relation to Short – Term Climatic Deterioration”, Quaternary Studies in Poland, 4, 189 – 198.
  • Rose, J. (1995) “Lateglacial and Early Holocene River Activity in Lowland Britain”, Palaoklimaforschung, 14, (in press).
  • Ruegg, G. (1993) “Alluvial Architecture of the Quaternary Rhine – Meuse River System in the Netherland”, Geologie en Mijnbouw, 72, 321- 330.
  • Schumm, S. (1979) “Geomorphic Thresholds: The Concept and its Applications”, Transcations Institute British Geographers, 4, 485 – 515.
  • Soergel, W. (1939) “Das Diluviale System”, Fortschritte Geologie und Paleontologie, XII – 9, 1 – 92.
  • Vandenberghe, J. (1995) “Postglacial River Activity and Climate: State-Of-The-Art And Future Prospects”, Palaoklimaforschung, 14, (in press).
  • Vandenberghe, J. and Van Huissteden, J. (1988) “Fluvio – Aeolian İnteraction in a Region of Continous Permafrost”, Proceedings of the 5th International Conference on Permafrost, 1, 876 – 881.
  • Vandenberghe, J., Mommersteeg, H. and Edelman, D. (1993) “Lithogenesis And Geomorphological Processes of the Pleistocene Deposites At Maastricht – Belvedere”, Mededelingen Rijks Geologische Dienst, 47, 7 – 17.
  • Vandenberghe, J., Kasse, C., Bohncke, S. and Kozarski, S. (1994) “Climate – Related River Activity at the Weichselian – Holocene Transition: A Comparative Study of the Warta and Maas Rivers”, Terra Nova, 6, 476 – 485.
  • Van Geel, B., Coope, R. G. and Van Der Hammen, T. (1989) “Palaeoecology and Stratigraphy of the Lateglacial Type Section at Usselo (The Netherlands)”, Reviews of Palaeobotany and Palynology, 31, 359 – 448.
  • Van Huissteden, J. and Vandenberghe, J. (1988) “Changing Fluvial Style of Periglacial Lowland Rivers During the Weichselian Pleniglacial in the Eastern Netherlands”, Zeitschrift für Geomorphologie, Supplement Band, 71, 131 – 146.
  • Van Kolfschoten, T., Roebroeks, W. and Vandenberghe, J. (1993) “The Middle and Late Pleistocene Sequence at Maastricht – Belvedere: The Type Locality of the Belvedere Interglacial”, Mededelingen Rijks Geologische Dienst, 47, 81 – 91.
  • Veldkamp, A. and Kroonenberg, S. (1993) “Late Quaternary Chronology of the Allier Terrace Sediments (Masif Central, France)”, Geologie en Mijnbouw, 72, 179 – 192.
There are 23 citations in total.

Details

Other ID JA72UE97TZ
Journal Section Research Article
Authors

J. Vandenberghe This is me

Uğur Doğan

Erdem Bekaroğlu C. This is me

Publication Date August 1, 2005
Published in Issue Year 2005 Volume: 3 Issue: 2

Cite

APA Vandenberghe, J., Doğan, U., & Bekaroğlu C., E. (2005). ZAMAN, İKLİM VE AKARSU GELİŞİMİ. Coğrafi Bilimler Dergisi, 3(2), 70-80. https://doi.org/10.1501/Cogbil_0000000058