Organizational change : problems and prospects for internal consultants

This paper develops a broad conceptual framework for internal change agents in organizations. It considers a range of important factors in the organization which are postulated to influence the form and progress of change, and also provides a critical analysis of relevant theoretical approaches to the dilemmas and opportunities posed by these factors. There is no treatment of specific organization development strategies or techniques. Rather, the objectives are to discuss in terms applicable to a variety of organizations, some of the critical situational variances facing internal change agents and to establish some principles and guidelines which may assist them in planning for change

Nuclear factor I genes regulate neuronal migration

Neuronal migration plays a central role in the formation of the brain, and deficits in this process can lead to aberrant brain function and subsequent disease. Neuronal migration is a complex process that involves the interaction of the neuron with the surrounding environmental milieu, and as such involves both cell-intrinsic and cell-extrinsic mechanisms. Studies performed in rodent models to investigate the formation of brain structures have provided key insights into how neuronal migration is coordinated during development. Within the cerebral cortex, glutamatergic neurons derived from the cortical ventricular zone migrate radially into the cortical plate, whereas interneurons derived within the ventrally located ganglionic eminences migrate tangentially into the cortex. Within the embryonic cerebellum, cerebellar granule neuron progenitors migrate from the rhombic lip over the surface of the cerebellar anlage, before differentiating and migrating radially into the internal granule layer of the cerebellum perinatally. In this review, we focus on one family of proteins, the nuclear factor I transcription factors, and review our understanding of how these molecules contribute to the formation of the hippocampus and the cerebellum via the regulation of neuronal migration

Global Microwave Imager (GMI) Spin Mechanism Assembly Design, Development, and Performance Test Results

The GMI Spin Mechanism Assembly (SMA) is a precision bearing and power transfer drive assembly mechanism that supports and spins the Global Microwave Imager (GMI) instrument at a constant rate of 32 rpm continuously for the 3 year plus mission life. The GMI instrument will fly on the core Global Precipitation Measurement (GPM) spacecraft and will be used to make calibrated radiometric measurements at multiple microwave frequencies and polarizations. The GPM mission is an international effort managed by the National Aeronautics and Space Administration (NASA) to improve climate, weather, and hydro-meteorological predictions through more accurate and frequent precipitation measurements [1]. Ball Aerospace and Technologies Corporation (BATC) was selected by NASA Goddard Space Flight Center (GSFC) to design, build, and test the GMI instrument. The SMA design has to meet a challenging set of requirements and is based on BATC space mechanisms heritage and lessons learned design changes made to the WindSat BAPTA mechanism that is currently operating on-orbit and has recently surpassed 8 years of Flight operation

Upper Mantle Pollution during Afar Plume-Continental Rift Interaction

International audienceNew Pb, Sr, Nd, Hf, and He isotope data for Quaternary basalts, erupted from Debre Zeyit, Butajira, and the Wonji Fault Belt of the Main Ethiopian Rift, show systematic mixing relationships involving three distinct mantle sources. The Pb, Sr, Nd, and Hf isotopic arrays converge in a specific region of isotopic multi-space where they define the composition of the Afar mantle plume (centered about (206)Pb/(204)Pb = 19 center dot 5, (87)Sr/(86)Sr = 0 center dot 7035, epsilon(Nd) = +4 center dot 6, epsilon(Hf) = +9 center dot 3, (3)He/(4)He > 15 R(A)). This plume end-member has an identical composition to that observed previously in oceanic basalts. The distinct isotopic arrays for the various volcanic areas in the Main Ethiopian Rift vary spatially in a systematic manner, and may be viewed as pseudo-binary mixing arrays. This further suggests that the Afar mantle plume interacts with the local continental lithosphere and upper mantle asthenosphere (mid-ocean ridge basalt-like source) through an ordered sequence of mixing events. Simple mixing models require that the mass proportions of continental lithosphere and upper mantle involved in magma generation must be nearly constant within each volcanic area, but that the proportion of plume material decreases regularly with distance southwestward along the Main Ethiopian Rift, away from the central axis of the plume. This systematic behavior means that continental lithosphere can become detached and mixed into the shallow mantle prior to the flow of upwelling plume material beneath the developing rift system. Detachment and mixing into the asthenosphere during continental rift evolution is an important process for producing the range of ambient upper mantle compositions sampled by mid-ocean ridge volcanism away from island hotspots