效果
发表于 2025-3-27 00:44:55
http://reply.papertrans.cn/71/7006/700520/700520_31.png
atopic-rhinitis
发表于 2025-3-27 03:39:09
Malcolm J. Bowman,Richard L. Iversonls, Kettmann und Nolte (1986). Auch bei ihnen waren lediglich 12% der Befragten supervisionsunerfahren. Insgesamt 99% derjenigen, die in dieser Studie zur Frage der Bedeutung der Supervision Stellung nahmen, bewerteten sie als „Hilfe“. Lediglich 1% der Befragten gab an, daß Supervision „nicht effekt
花束
发表于 2025-3-27 06:54:20
http://reply.papertrans.cn/71/7006/700520/700520_33.png
神圣不可
发表于 2025-3-27 10:29:44
http://reply.papertrans.cn/71/7006/700520/700520_34.png
Condyle
发表于 2025-3-27 17:33:52
http://reply.papertrans.cn/71/7006/700520/700520_35.png
Jargon
发表于 2025-3-27 19:34:45
Biological Aspects of the Nova Scotian Shelfbreak Frontsed that frontal convergences resulted in localized accumulations of plankton and particulate materials which in turn attracted higher levels in the food chain--a fact fully exploited by Japanese fishermen.
全部逛商店
发表于 2025-3-27 23:37:21
http://reply.papertrans.cn/71/7006/700520/700520_37.png
recession
发表于 2025-3-28 03:26:55
Frontal Dynamics and Frontogenesisce the cross-stream circulation in such a case. It is possible to formulate time-dependent models for the genteration of fronts (frontogenesis) which are time-dependent and non-dissipative, but steady-state front models and models for annihilation of fronts (frontolysis) require dissipation.
拖网
发表于 2025-3-28 06:47:39
Physical Aspects of the Nova Scotian Shelfbreak Fronts properties across this front is clearly important to any consideration of overall budgets for mass transfer in this area, and it was suggested that processes at the front might give rise to a vertical transport of nutrients to help account for the high productivity in the warm surface slope water (Fournier ., 1977).
腼腆
发表于 2025-3-28 10:31:23
Headland Frontshallow sea fronts (see section 5) is their short characteristic length and time scales. Typically, headland fronts may be expected to go through a generation and dissipation phase within a tidal period. Consequently, if the dissipation is complete, the length scales for headland fronts will not exceed a tidal excursion.