By R.Z. Xi, Wei-Zu Gu, Klaus-Peter Seiler
In the 20 th century, water administration excited by the neighborhood scale of curiosity. within the twenty first century we are going to be dealing with adjustments within the volume of our water cycle. The forces in the back of those new demanding situations are industrialisation, inhabitants development and an insufficiently quick reaction to climatic switch. The value and distribution of world alterations will not be precisely predictable, simply because we are living in an ever-changing atmosphere and are confronted with severe and interacting techniques, which all will not be but sufficiently understood. consequently, to shoulder this activity, hydrology may still embody extra integrative and interdisciplinary methods and accomplish extra flexibility in tests and judgements. to higher confront this problem, catchment-related suggestions are extra vital than neighborhood options, to fulfill the water call for of agriculture, ecosystems, and the non-public area. it really is clever to bear in mind that the surroundings has a "sustainable reminiscence" and our wisdom approximately attenuation capacities and resilience of our environment remains to be low.
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Extra resources for Research Basins and Hydrological Planning: Proceedings of the International Conference, Hefei/Anhui, China, 22-31 March 2004
Sample text
2 East Asia – Japan According to Sakaguchi (1982, 1983) the period between 2270 and 2090 BC was warm. He named it – 1st Late Jomon warm stage. It continued to be warm to 1460 BC. During this period there is evidence for high sea levels starting ca. 3 BP and ending ca. 5K BP. The evidences are reported by Sakaguchi (1983), who correlates it with his pollen climatic changes curve and archaeological sites. Pirazzoli and Delibrias (1983) who investigated late Holocene and recent sea level changes in Kume Island, claimed that the maximum transgression occurred around 4K BP.
There was a concurrent encroachment of sand dunes into the coastal plain of Israel. Issar (2003) refers to this warm and dry period as the Moslem–Arab period. 2 East Asia – Japan From Sakaguchi’s (1983) palynological diagram it is evident that the Nara Heran Kamakura warm stage ending at ca. 1300 AD was followed by the cold Little Ice age, which continued, albeit with short term fluctuations until 1900 AD. A warm episode occurred at ca. 1840 AD, and an extremely cold episode around 1890, during which storms were abundant and rice harvests were low, leading to famine and rebellion.
Bull. Dept. Geogr. Univ. Tokyo, No. 15, 63–76 Raban, A. and Galili, E. (1985). Recent maritime archaeological research in Israel – A preliminary report. The International Journal of Nautical Archaeology and Underwater Exploration, 14(4), 321–356 Sakaguchi, Y. (1982). Climatic variability during the Holocene epoch in Japan and its causes. Bull. Dept. Geogr. Univ. Tokyo, 14, 1–27 Sakaguchi, Y. (1983). Warm and cold stages in the past 7600 years in Japan and their Global Correlation. Bull. Dept. Geogr.