Pingo Apk
Clarabella Doom
Another name for a pingo is a hydrolaccolith. A pingo is usually a bump shape or cone shape with a core of ice beneath the soil. Pingos apparently even grow taller over time, especially when they are new. The pingos in the Seward Peninsula often exist on or in the middle of an otherwise flat, wide area of the tundra.
Whenever you refresh the web page PINGO_IP/pingo (replace PINGO_IP with the value you've got earlier), Pingo shows the time, and nine different styles to pick from. You can set the alarm and adjust the brightness. The save button stores your preferences in non-volatile memory, so Pingo will remember those if it reboots.
I have dedicated Tuesday to Pingo. I replaced the signal wire to ring 9, and touched up a couple of other spots. I have used my ohm-meter everywhere, getting 0 or single digit ohm readings. A success on ring 9!!! Pingo starts up well, with the classic clock face, but then it goes back to weird shit. Figured that out. One leg of the capacitor needed to be soldered more securely. *Much* less weirdness. Classic, modern, ringed, and minimal work! Frantic, static, tricky and pingo still have dancing ring 4. Ring 5 is almost always off, but sometimes is half-lit. Here's where I went off the deep end. I moved my Vin wire from the NodeMCU Vin pin over to my RSV pin which is where your VU pin is. Uploading the sketch caused me to have to reboot my PC.
Question 1: Are you *sure* ring 4 is off, not ring 5?
Question 2: What's next, after putting Vin back?
I may put Pingo together and only use the classic, modern, ringed and minimal settings. ;-)
BTW, might I see you at Makers Central next weekend in Birmingham?
Yup. Baud rate in the sketch is 74880. Now I get English alphabet! Thanks. Next brick wall is that my 'IP address'/pingo won't connect. I've tried my Android phone and both browsers on my Windows PC. I have no proxy. My antivirus and firewall look like they should be okay.
I didn't know they removed the free tier. The key used in the code still works, and if it is only used by pingo clocks it should work for the first couple of hundred clocks just fine. But you are right, you can/should replace the key in the code with your own. (I did contact openweathermap before I made the key part of the code, and their answer was that it was ok to do so).
Mars, Ceres, and the Earth have abundant reserves of ground ice. On Earth, ice-cored mounds known as pingos are important indicators of extant and extinct near-surface groundwater systems, hydrogeologic properties, and local climate.
Spacecraft observations of Mars and Ceres have revealed a variety of deca- to kilometer scale hills with morphological similarities to terrestrial pingos in ice-rich environments. Domes observed on Europa, Ganymede, and Callisto also resemble these ice-cored structures.
Pingo STARR will advance human and lander scale geophysical techniques specifically tailored to detect, characterize, and investigate the cryohydrology and genesis of possible pingo-like features on Earth, Mars, and Ceres. This systems-level field campaign will be the most comprehensive to date for any terrestrial pingos, and the first dedicated analysis of pingos from a planetary science perspective. Our science and technology objectives will provide valuable insight into detecting and characterizing ground -ice and -water systems on Mars and Ceres.
You sometimes hear pingo used interchangeably with the equally fun-to-say hydrolaccolith (another spellcheck reject). Some geomorphologists, however, use the former to refer to perennial ice formations, while hydrolaccoliths can melt and reform seasonally.
The Pingo Canadian Landmark protects a unique arctic landform: ice-cored hills called pingos. Rising out of the flat tundra, pingos provide a distinctive backdrop to the community of Tuktoyaktuk, Northwest Territories.
The Pingo Canadian Landmark features 8 of the 1350 pingos found in the region, including Ibyuk Pingo. Ibyuk is Canada's tallest and the world's second-tallest pingo. It reaches 49 metres (about 161 feet) in height and stretches 300 metres (about 984 feet) across its base.
Other than gigantic Ibyuk, the pingos in Pingo Canadian Landmark range from five meters to 36 metres tall. They represent different stages of growth, from budding newborns to elder pingos that are shrinking and slumping.
For eons, the Inuvialuit of the Arctic coast have used pingos as navigational aides. They also serve as a useful lookout when searching the tundra for caribou or scanning the sea for seals and whales.
homeupdatesmapphotosalsapperscontactabout Mt. Pingo Ski HillLate 1970's to Mid 1990's Name of Ski Area: Mt. Pingo, Mt. Prudhoe Location: Prudhoe Bay, 200 yards to the south of Spine road between British Petroleum's (BP) Base Operations Center (BOC) and Gathering Center 1 (GC1) Type of Area: Ski Hill Dates of Operation: Late 1970's to Mid 1990's ???? Who Built It?: Natural ski slope. No trees for 100 miles. This hill is a pingo - a mound found in arctic regions that consists of soil covering a bulging cell of permafrost (ice). Base / Vertical: Base: 15' / Vertical: 15' Facilities: Oil production facilities are nearby that support the largest oil field in the United States. History: [Tim Kelley] When I first went to the North Slope of Alaska in 1986 (the oil fields between the north slope of the Brooks Range and the Arctic Ocean) I was working at BP's Base Operations Center (BOC). The BOC had a sundries shop and I noticed they sold T-shirts with a skier descending a small hill and the logo: "Ski Mt. Pingo" !
I looked on Wikipedia to find out what a pingo is. Very interesting. Then I made a donation to Wikipedia. I came back to this e-mail from Wilderness Watch, which I enjoyed reading and viewing, and made a donation. Keep up the good work!
Ibyuk Pingo, which is 49 m high and 300 m in basal diameter, is one of the largest pingos in the world. Precise surveys carried out for the 1973 to 1983 period indicate that the lower half of the pingo, below a height of 25 m, shows no perceptible growth. From 25 m to the top, the growth steadily increases to a maximum of 2.3 cm/yr at the summit. The source of growth is believed to lie at a depth of about 65 m below the highest peak. Evidence based upon the depth of permafrost near the pingo, radiocarbon dating of wood in the pingo overburden, heat conduction theory, and the measured growth rate suggests an age of about 1300 200 yr. Ibyuk Pingo is in an unstable state and collapse could be initiated by further slumping, a thermal disturbance to the crater, or erosion along a radial dilation crack. A study of the potential collapse pattern of Ibyuk Pingo suggests a number of criteria that might be employed in the environmental reconstruction of large circular features that might be identified as collapsed pingo remnants.
Field studies of pingo ice show that alternating clear and bubble bands may grow when water freezes at the top of a subpingo water lens. A study of the banding at one excellent exposure of pingo ice shows that the clear bands probably grew during propagation of the cold winter temperature waves, the bubble bands, from the warmer summer temperature waves. The likely cause for the gradual transitions from clear to bubble bands followed by the abrupt transitions from bubble to clear bands was marked asymmetry of the periodic temperature waves in permafrost overlain by an active layer whose thermal properties varied seasonally. Pingo growth, as determined from the growth of bands, shows good agreement with Stefan's equation where growth varied as the square root of time. Geochemical profiles show no systematic change with depth. Stable-isotope profiles for δ18O and δD show linear trends with depth and a depletion of the heavy isotopes. The co-isotope slope of 7.2 suggests freezing, with the input being impoverished in the heavy isotopes.
In a region of subsidence, as recent sediments pass through the base of permafrost, compaction becomes possible. The resulting water expulsion produces an artesian head responsible for building pingos.
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