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Titlebook: Learning in Communities; Interdisciplinary Pe John M. Carroll Book 2009 Springer-Verlag London 2009 CSCW.Collaborative Learning.Community n

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21#
發(fā)表于 2025-3-25 05:46:43 | 只看該作者
22#
發(fā)表于 2025-3-25 08:19:10 | 只看該作者
Patterns as a Paradigm for Theory in Community-Based Learninggularities of practices in ways that are potentially intelligible, verifiable, and perhaps useful to the practitioners themselves. We present two example patterns and discuss issues and directions for developing patterns as a theoretical foundation for community-based learning.
23#
發(fā)表于 2025-3-25 13:45:28 | 只看該作者
24#
發(fā)表于 2025-3-25 17:18:35 | 只看該作者
Supporting Community Emergency Management Planning Through a Geocollaboration Software Architecture emergency plans and procedures. Issues such as emergency vehicle traffic routes and staging areas for command posts, arriving media, and personal first responders’ vehicles must be agreed upon prior to an emergency event to ensure an efficient and effective response. This work presents a software a
25#
發(fā)表于 2025-3-25 20:21:28 | 只看該作者
26#
發(fā)表于 2025-3-26 01:04:16 | 只看該作者
27#
發(fā)表于 2025-3-26 04:40:27 | 只看該作者
Lynette Kvasny is enormous interest in trying to work out the mechanisms which trigger ice ages to begin, and what causes them to end. Of particular interest is the fact that ice ages appear to begin and end very abruptly on the geological timescale. ...Previous and existing books on ice ages are mostly short, po
28#
發(fā)表于 2025-3-26 09:15:46 | 只看該作者
29#
發(fā)表于 2025-3-26 12:45:08 | 只看該作者
Murali Venkatesh,Jeffrey S. Owenscial matures, sea level remains high. Ice may start accumulating around 65°N latitude after 5500?years, but the initial impact on sea level is small. If the duration of an Interglacial is defined by sea level, it will certainly be much longer than 5500?years. If an Interglacial is defined as the per
30#
發(fā)表于 2025-3-26 20:10:48 | 只看該作者
ure signal is described. Dating the layers in an ice core is a difficult matter, and a number of techniques have been employed. Counting annual layers visually is the most straightforward, but this method is limited to more recent times. Other, more sophisticated methods are described in the text. U
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