A problem for regular (single-board) RMA shims is that we have to create separate per-board RMA shims for each project, which makes it hard to manage shim images and physical USB drives. A universal shim contains multiple RMA shims for different boards, which is easier to manage and distribute.
The RMA shim has a menu that allows the user to select an action to perform, which is described in Factory Installer README. Moreover, if the RMA shim is created using image_tool rma create command, the tool adds a flag RMA_AUTORUN=1 in lsb-factory file, which sets the default action of the menu depending on the cr50 version and hardware write protection status, such that:
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During installation, you can remove the RMA shim when the copy is complete (the text color changes from yellow to green). After the installation, the device will boot into the test image with factory toolkit. Run through the factory tests to complete the flow. The last test should wipe out the factory test image and enable the release image.
image_tool rma merge supports merging universal shims. If there are duplicate boards, it will ask the user to select which one to use. It can be used to update a board in a universal shim using an updated single-board RMA shim.
Nongshim Tako Chips are octopus flavored chips that are as fun to look at as they are to eat. Crispy tako chips come in cute octopus shapes, and their savory and salty flavor is reminiscent of grilled octopus.
Marko Testing Library is not dependent on any test runner. However, it isdependent on the test environment. This package works for testing both serverside, and client-side Marko templates and provides a slightly differentimplementation optimized for each. This is done using abrowser shim,just like in Marko.
For client-side testing of your components with Mocha often you will use abundler to build your tests (this will properly resolve the browser shimsmentioned above) and then you can load these tests in some kind of browsercontext.
First you need to download a SH1MMER bin. Download a shim at dl.sh1mmer.me, and build (modify) it with the SH1MMER web builder.
Once you've obtained a MODIFIED SHIM (NOT A RAW SHIM), you can continue.
In the eight-episode series, the three -- Yoo Jae-suk, Lee Kwang-soo and Kim Yeon-koung -- get a hands-on experience in eight different fields ranging from making traditional Korean roof tiles and fermented Korean sauces to catching long-legged octopus on a mud flat and to weaving fine ramie.
An RMA (return merchandise authorization) shim is a factory tool designed to be used by mostly repair centers for resetting chromebooks,changing their serial numbers, running tests, etc. In theory it would be able to wipe enrollment.The shim itself is a .bin file similar to a recovery image which you then flash to a usb that can be plugged into chromebooks to boot it.These shims are kept confidental by chromebook manufacturers and one that is officially signed (meaning it works on any chromebook without enabling unsigned boot) should never end up in the hands of an end user, so we struggled to obtain them.
First you would install chromebrew on a normal devbook and shove its files into a compressed archive, take the shim image and create a brand new 13th partition,filling it in with the contents of chromebrew.Upon boot of the RMA shim, the 13th partition can be mounted over /usr/local,giving the shell scripts accesss to whatever software we install.
Once the firmware update hits, every single shim usb in the world would suddenly stop working, requiring the repair centers to get them from the manufacturers, and the manufacturers to get a bunch of from google. Overall, a large logistical issue.
To shutdown the Pi I'm using the pimoroni on-off-shim ( -shim?variant=41102600138). With a push-button in the printers skirt I can turn on and off the printer and since the pimoroni cuts power on shutdown it can also be shut down by software from klipper.
Bathymetry and schematic circulation pattern of the Korea Strait and neighboring sea. TC and KSBCW denote the Tsushima Current and the Korea Strait bottom cold water. Study area is marked by a rectangular box. Depths are in meters
Hydrographic studies show the seasonal variation of the East Korean Warm Current (EKWC), which is a branch of the Tsushima Current along the Korean coast. To understand the dynamics of the branching mechanism of the TC in the Korea Strait, a hydraulic model with two active layers was investigated in a rectangular strait with varying depth. When the lower cold water flows southward in a shallow meridional channel from the deep northern basin, it separates from the eastern boundary because of the sloping bottom to conserve potential vorticity. After separation, the lower layer hugs the western boundary as the channel becomes shallow. In a region where the lower layer is absent due to separation, the northward flow in the upper layer has a positive relative vorticity to conserve potential vorticity because the bottom topography becomes deeper from south to north. The northward velocity has its maximum on the eastern boundary. This mechanism may explain the formation of the branch along the Japanese coast. The upper layer along the western boundary experiences shrinking of its water column because of the presence of the lower layer, and negative relative vorticities are induced to conserve potential vorticity. The negative relative vorticity intensifies the northward flow of the upper layer near the western boundary. This is believed to be the causal mechanism of the EKWC. If the top of the lower layer in the basin is deep, such as it is in winter, the lower layer cannot reach the strait since the Bernoulli potential of the lower layer is small. This may explain why the EKWC is absent in winter.
However, Kim and Legeckis (1986) show that the EKWC is sometimes absent, and Isoda and Saitoh (1993) suggest that the formation of the EKWC is seasonal. Cho and Kim (1996) confirm the seasonality of the EKWC and suggest the possibility that the southward movement of Korea Strait bottom cold water (KSBCW) is responsible for the formation of the EKWC. Furthermore, Cho and Kim (1996) show that the change of potential vorticity due to the shrinking of the Tsushima warm water (TWW) along the Korean coast is greater than the planetary beta effect. Isobe (1994, 1997) also argues that the JEBAR effect in Korea Strait, which is caused mainly by cold water along the Korean coast in summer, supplies the negative vorticity. The absence of the EKWC bears an exceptional importance in terms of not only the branching mechanism but also the circulation in the East Sea. ff782bc1db
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