We’re trashing the planet. Everyone gets that, right? I’ve written several posts about trash, debris, and refuse littering and orbiting the planet, one of which is arguably among my greatest hits owing to the picture below showing The Boneyard outside Tucson, Arizona. That particular scene no longer exists as those planes were long ago repurposed.
I’ve since learned that boneyards are a worldwide phenomenon (see this link) falling under the term urbex. Why re-redux? Two recent newbits attracted my attention. The first is an NPR article about Volkswagen buying back its diesel automobiles — several hundred thousand of them to the tune of over $7 billion. You remember: the ones that scandalously cheated emissions standards and ruined Volkswagen’s reputation. The article features a couple startling pictures of automobile boneyards, though the vehicles are still well within their usable life (many of them new, I surmise) rather than retired after a reasonable term. Here’s one pic:

The other newsbit is that the Great Pacific Garbage Patch is now as much as 16 times bigger than we thought it was — and getting bigger. Lots of news sites reported on this reassessment. This link is one. In fact, there are multiple garbage patches in the Pacific Ocean, as well as in other oceanic bodies, including the Arctic Ocean where all that sea ice used to be.
Though not specifically about trashing the planet (at least with trash), the Arctic sea ice issue looms large in my mind. Given the preponderance of land mass in the Northern Hemisphere and the Arctic’s foundational role in climate stabilization, the predicted disappearance of sea ice in the Arctic (at least in the summertime) may truly be the unrecoverable climate tipping point. I’m not a scientist and rarely recite data or studies in support of my understandings. Others handle that part of the climate change story far better than I could. However, the layperson’s explanation that makes sense to me is that, like ice floating in a glass of liquid, gradual melting and disappearance of ice keeps the surrounding liquid stable just above freezing. Once the ice is fully melted, however, the surrounding liquid warms rapidly to match ambient temperature. If the temperature of Arctic seawater rises high enough to slow or disallow reformation of winter ice, that could well be the quick, ugly end to things some of us expect.