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Titlebook: Next Generation Wireless Networks; Sirin Tekinay Book 2002 Springer Science+Business Media New York 2002 ATM.Broadband Wireless Access.Hos

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發(fā)表于 2025-3-23 11:33:53 | 只看該作者
Next Generation Wireless Networks978-0-306-47310-4Series ISSN 0893-3405
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發(fā)表于 2025-3-23 15:43:50 | 只看該作者
0893-3405 and location enhanced applications and services that will give wireless systems the competitive edge over others. The main theme of the book is the advent of wi978-1-4757-7411-5978-0-306-47310-4Series ISSN 0893-3405
13#
發(fā)表于 2025-3-23 19:33:39 | 只看該作者
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發(fā)表于 2025-3-24 01:09:16 | 只看該作者
Wireless Broadband Multimedia and IP Applicatins via Mobile ATM Satellites,r the future multimedia personal terminals, thus, there is a requirement of integration of all these telecommunications technologies. Wireless ATM came to integrate the cell-switched ATM facilities in wireless environment and mobile IP has a similar goal for IP networks. IP over ATM also proposed to
15#
發(fā)表于 2025-3-24 04:49:07 | 只看該作者
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發(fā)表于 2025-3-24 10:19:18 | 只看該作者
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發(fā)表于 2025-3-24 14:32:31 | 只看該作者
18#
發(fā)表于 2025-3-24 15:11:47 | 只看該作者
urfaces have been interpreted and parameterized in terms of Monin-Obukhov similarity theory. The ocean has two unique properties that have greatly simplified this approach: the surface humidity is assumed to be in equilibrium with the saturation vapor pressure at the ocean surface temperature and th
19#
發(fā)表于 2025-3-24 22:38:16 | 只看該作者
Ana Lúcia Iacono,Christopher Roseurfaces have been interpreted and parameterized in terms of Monin-Obukhov similarity theory. The ocean has two unique properties that have greatly simplified this approach: the surface humidity is assumed to be in equilibrium with the saturation vapor pressure at the ocean surface temperature and th
20#
發(fā)表于 2025-3-24 23:47:15 | 只看該作者
Abbas Jamalipouring this principle. Basing on this remark, an equation can be obtained to calculate the associated energy velocity. This intrinsic equation only refers to complex Christoffel equation. Limiting the study to principal planes and plotting the associated complex wave surface, it can be shown that four
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