Little Known Hikes: Wind In The Pines And Falls Creek – The Sheet In 3 Sheets To The Wind Crossword

Spoil In The Fridge Crossword

Sun, 21 Jul 2024 00:13:11 +0000

Perhaps the bear didn't approve of being spied on, I will never know. Send me a message on Facebook or Instagram, or email me at I really hope this recording brings you a little peace and provides you with a brief respite from the many stresses of everyday life. Wind in the Pines Preserve & Falls Creek SNA. Episode 39: Dripping Ice Cave. Unfortunately lightning strikes from these storms caused several wildfires which forced the closure of Lava Beds National Monument and a mandatory evacuation of the Medicine Lake Area in the days following the date of this recording. I hope you don't mind it too much. If you have any comments or questions you can email the podcast at You can also get in touch by visiting my website- I hope that this or any of my recordings can provide you with a little peace amidst the tumult of this chaotic, stressful, and crazy world we all live in together. I set up a microphone beside Water Strider Creek, and while it recorded I hiked south to Butcherknife Creek, then made this recording on my way back.

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Wind In The Pines Nature Park Wisconsin

It was a blustery day which started off sunny, but by afternoon clouds gathered and it began to rain as I wandered around the forest, across streams, and through small meadows. This podcast is independently produced and is made possible in part by the generous support of listeners like you. This was recorded at a spring fed mountain stream on a summer afternoon in the Trinity Mountains, a subrange of the Klamath Mountains, in Siskiyou County, California. PEACE FOR UKRAINE NOW!!! Finding them is half the fun and exploring with your family and friends is even better! The recording starts well before dawn at around 2:30 a. m. and continues through sunrise till around 7:00 a. Luckily, I was able to capture two subsequent thunderclaps in the snow, which I present to you.

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112: Distant Thunder At Shastine Crater. Open 4 am - sunset daily. I left my recording rig in an Aspen thicket at the edge of the meadow to record all day, and went to retrieve it at sunset. A breezy sunset at Soberanes Point in Garrapata State Park, Monterey County, California. I hope this or any of my recordings are able to provide you with a bit of peace during this ongoing crisis. The recording starts beside Butcherknife Creek, then follows the trail north to Water Strider Creek. This was recorded at a snowmelt stream near Porcupine Lake in the Shasta-Trinity National Forest, Siskiyou County, California. Episode 1: Waterfall. Mountain Chickadees and Red Breasted Nuthatches can be heard in the background, and a pair of curious Ravens fly by to see what all the ruckus is about. This was recorded on a clear late summer morning beside Bumpass Creek just below the Bumpass Hell geothermal area in Lassen Volcanic National Park, Shasta County, California. Recently your contributions have helped me purchase materials to make wind protection for my microphone, you can see pictures of my handiwork on my Instagram.

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If you appreciate natural sound that has been thoughtfully gathered and is entirely free from advertising, I hope that you will consider supporting the podcast. The war crimes and atrocities committed against the people of Ukraine are truly sickening and I hope those responsible are held fully accountable for their heinous and unconscionable actions. Deep snow covered the ground and much of the creek, though some stretches were exposed at the bottom of deep channels which had formed in the snow above the creek and allowed the sound of trickling water and dripping snowmelt to be heard from above. There was a lot of air traffic on the day I recorded, and the least noise polluted part of the recording happened on a section of trail which had some uphill parts, so you can hear me breathing a bit. As an aside, I did have an interesting Black Bear encounter while I was there. If anyone else would like to contribute, click the support link at the end of this description.

Wind In The Pines

I would also like to give a special thanks to listener Leah who so kindly sent a generous donation to the podcast by mail. The recording starts just after sunset as the birds were singing their last songs of the day and the frogs were warming up for their nightly chorus. I aim to provide you with a break from the anthropocentric world, and nothing could be more anthropocentric than Facebook and social media in general. This was recorded on a cloudy spring afternoon just above the base of Mount Shasta in a stand of old growth trees near Squaw Valley Creek, Shasta-Trinity National Forest, Siskiyou County, California. This recording was gathered on a clear spring day at the confluence of two mountain streams high in the upper watershed of the Middle Fork of the Sacramento River. Episode 60: Crisp Winter Day at a Secluded Meadow. The wind ripples on the open water were pushing bits and pieces of broken ice against the edge of the frozen half of the lake, which created some interesting sounds. Send me a message on Facebook or Instagram, or email me at Please do all you can to make the world a more peaceful and sustainable place for all living things.

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There is some air traffic on this recording. This was recorded on a clear and cool winter day while I paddled a canoe on Lake McCloud in Shasta-Trinity National Forest, Shasta County, California. This was recorded on a sunny afternoon at Butcherknife Creek near the Pacific Crest Trail in Shasta-Trinity National Forest, Shasta County, California. You can learn more about it here- It was a cool and breezy morning and I have to confess there weren't quite as many birds on this morning as I have heard at this location in the past.

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Episode 94: Mount Shasta- Gusty Winter Wind Near Sand Flat. It was a refreshingly crisp spring morning, with a thin blanket of recently fallen spring snow covering the banks of the river. I was further disheartened when I was charged a hefty returned payment fee by the company which handles online payment processing for my website. The second part is a large flock roosting in, and moving between, willow trees and is nine minutes long. This was recorded on a spring day on the south flank of Medicine Lake Volcano in the Medicine Lake Highlands near the edge of Chimney Crater, Shasta-Trinity National Forest, Siskiyou County, California. And if you have any questions or comments about the podcast you can email me at I truly hope you enjoy this or any of my recordings. I really want to thank my monthly supporters on both Anchor and Patreon, as well as those of you that have made one time donations. As our American election nears I hope you are keeping the Earth, our planet, our home, in mind as you head to the polls or complete your mail in ballot.

In this second part of the recording the wind picks up and the rain falls more heavily as the night passes by and morning draws near. Episode 65: Castle Crags Wilderness- Snowmelt Rain. Considering the length of this recording, four jets in four hours is not too bad. The roaring surf is heard in the background as small wind waves lap at the shore of the estuary. The occasional splash you'll hear are trout jumping. Located trailside on the Pacific Crest Trail, this beautiful spring is a convenient place to refill your water and take in the view of the Trinity Alps to the west, while also admiring the abundance of wild flowers and the odd looking California Pitcher Plant which grows in the pure and cold spring water as it cascades downslope from the spring. It was a cold, clear, moonlit night with a steady breeze blowing through the trees. Wed Jun 29 2022 at 05:30 pm to 09:00 pm. It was a beautiful day and I was very happy to get two recordings to share with you. I recorded this on the Winter Solstice at the confluence of a small cascading stream and the South Fork of the Sacramento River.

I know that the problems we deal with aren't the same, but I know that we are all dealing with something and that we all suffer in our own ways. Send me a message on Facebook or Instagram, or email me at This episode is dedicated to a very good friend of mine that recently died, Orion Gardner. 114: Lost Coast- Strong Wind And Rough Surf At Mattole Beach. If you don't have any loved ones, then hug yourself. She chose an excellent location to set up the microphone and recorder for an overnight recording. The first part is a large flock sitting in cattails lining the edge of a canal and is eight minutes long.

It's the best way to support the podcast because it provides me with a reliable resource which I can draw from to provide you with these recordings. 113: Lost Coast- Mattole River Estuary. It was a warm evening for the time of year, and though the sky was otherwise clear, the air was laden with smoke from the many wildfires burning across Northern California which imbued the evening light with a deep golden hue. Episode 33: San Mateo Point at High Tide.

The night was very windy and I was camped closer to a standing dead tree than I should have been, so I laid awake most of the night hoping that a branch or even the whole tree wouldn't blow down on my campsite. The air was still and the glassy surface of the lake perfectly reflected the stars above, which elicited the surreal sensation of paddling through the heavens. This was recorded on a windy evening just before sunset at Mattole Beach on the Lost Coast in Humboldt County, California. Dec 05, 2019 01:03:04. If you like what you hear, show some love! You can also help by rating and reviewing the podcast on Apple Podcasts, I really enjoy hearing what you think! This recording was gathered on a clear and sunny morning near Sand Flat on the southwest side of Mount Shasta in Shasta-Trinity National Forest, Siskiyou County, California. And be as compassionate as possible in as many ways possible. Here we have my recording rig falling into Lake McCloud.

There is, increasingly, international cooperation in response to catastrophe—but no country is going to be able to rely on a stored agricultural surplus for even a year, and any country will be reluctant to give away part of its surplus. The same thing happens in the Labrador Sea between Canada and the southern tip of Greenland. Europe's climate, obviously, is not like that of North America or Asia at the same latitudes.

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The Mediterranean waters flowing out of the bottom of the Strait of Gibraltar into the Atlantic Ocean are about 10 percent saltier than the ocean's average, and so they sink into the depths of the Atlantic. Within the ice sheets of Greenland are annual layers that provide a record of the gases present in the atmosphere and indicate the changes in air temperature over the past 250, 000 years—the period of the last two major ice ages. The discovery of abrupt climate changes has been spread out over the past fifteen years, and is well known to readers of major scientific journals such as Scienceand abruptness data are convincing. The last time an abrupt cooling occurred was in the midst of global warming. Coring old lake beds and examining the types of pollen trapped in sediment layers led to the discovery, early in the twentieth century, of the Younger Dryas. Unlike most ocean currents, the North Atlantic Current has a return loop that runs deep beneath the ocean surface. The sheet in 3 sheets to the wind crossword answer. Indeed, we've had an unprecedented period of climate stability. When that annual flushing fails for some years, the conveyor belt stops moving and so heat stops flowing so far north—and apparently we're popped back into the low state. It's the high state that's good, and we may need to help prevent any sudden transition to the cold low state. It would be especially nice to see another dozen major groups of scientists doing climate simulations, discovering the intervention mistakes as quickly as possible and learning from them.

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I call the colder one the "low state. " In almost four decades of subsequent research Henry Stommel's theory has only been enhanced, not seriously challenged. Although we can't do much about everyday weather, we may nonetheless be able to stabilize the climate enough to prevent an abrupt cooling. Thermostats tend to activate heating or cooling mechanisms abruptly—also an example of a system that pushes back. Alas, further warming might well kick us out of the "high state. " They were formerly thought to be very gradual, with both air temperature and ice sheets changing in a slow, 100, 000-year cycle tied to changes in the earth's orbit around the sun. I hope never to see a failure of the northernmost loop of the North Atlantic Current, because the result would be a population crash that would take much of civilization with it, all within a decade. We need more well-trained people, bigger computers, more coring of the ocean floor and silted-up lakes, more ships to drag instrument packages through the depths, more instrumented buoys to study critical sites in detail, more satellites measuring regional variations in the sea surface, and perhaps some small-scale trial runs of interventions. 5 million years ago, which is also when the ape-sized hominid brain began to develop into a fully human one, four times as large and reorganized for language, music, and chains of inference. Salt circulates, because evaporation up north causes it to sink and be carried south by deep currents. Feedbacks are what determine thresholds, where one mode flips into another. What is three sheets to the wind. To the long list of predicted consequences of global warming—stronger storms, methane release, habitat changes, ice-sheet melting, rising seas, stronger El Niños, killer heat waves—we must now add an abrupt, catastrophic cooling. Because water vapor is the most powerful greenhouse gas, this decrease in average humidity would cool things globally. This would be a worldwide problem—and could lead to a Third World War—but Europe's vulnerability is particularly easy to analyze.

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One of the most shocking scientific realizations of all time has slowly been dawning on us: the earth's climate does great flip-flops every few thousand years, and with breathtaking speed. Further investigation might lead to revisions in such mechanistic explanations, but the result of adding fresh water to the ocean surface is pretty standard physics. But sometimes a glacial surge will act like an avalanche that blocks a road, as happened when Alaska's Hubbard glacier surged into the Russell fjord in May of 1986. In 1984, when I first heard about the startling news from the ice cores, the implications were unclear—there seemed to be other ways of interpreting the data from Greenland. Twenty thousand years ago a similar ice sheet lay atop the Baltic Sea and the land surrounding it. A stabilized climate must have a wide "comfort zone, " and be able to survive the El Niños of the short term. We might create a rain shadow, seeding clouds so that they dropped their unsalted water well upwind of a given year's critical flushing sites—a strategy that might be particularly important in view of the increased rainfall expected from global warming. Keeping the present climate from falling back into the low state will in any case be a lot easier than trying to reverse such a change after it has occurred. Counting those tree-ring-like layers in the ice cores shows that cooling came on as quickly as droughts. It was initially hoped that the abrupt warmings and coolings were just an oddity of Greenland's weather—but they have now been detected on a worldwide scale, and at about the same time.

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These blobs, pushed down by annual repetitions of these late-winter events, flow south, down near the bottom of the Atlantic. Surprisingly, it may prove possible to prevent flip-flops in the climate—even by means of low-tech schemes. Oceans are not well mixed at any time. This produces a heat bonus of perhaps 30 percent beyond the heat provided by direct sunlight to these seas, accounting for the mild winters downwind, in northern Europe. This was posited in 1797 by the Anglo-American physicist Sir Benjamin Thompson (later known, after he moved to Bavaria, as Count Rumford of the Holy Roman Empire), who also posited that, if merely to compensate, there would have to be a warmer northbound current as well. In the Greenland Sea over the 1980s salt sinking declined by 80 percent. The most recent big cooling started about 12, 700 years ago, right in the midst of our last global warming. A slightly exaggerated version of our present know-something-do-nothing state of affairs is know-nothing-do-nothing: a reduction in science as usual, further limiting our chances of discovering a way out. Water that evaporates leaves its salt behind; the resulting saltier water is heavier and thus sinks. Thus we might dig a wide sea-level Panama Canal in stages, carefully managing the changeover. This El Niño-like shift in the atmospheric-circulation pattern over the North Atlantic, from the Azores to Greenland, often lasts a decade.

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We can design for that in computer models of climate, just as architects design earthquake-resistant skyscrapers. Perish in the act: Those who will not act. We could go back to ice-age temperatures within a decade—and judging from recent discoveries, an abrupt cooling could be triggered by our current global-warming trend. These days when one goes to hear a talk on ancient climates of North America, one is likely to learn that the speaker was forced into early retirement from the U. Geological Survey by budget cuts. Sometimes they sink to considerable depths without mixing. Another sat on Hudson's Bay, and reached as far west as the foothills of the Rocky Mountains—where it pushed, head to head, against ice coming down from the Rockies. Sudden onset, sudden recovery—this is why I use the word "flip-flop" to describe these climate changes. But the regional record is poorly understood, and I know at least one reason why. Oslo is nearly at 60°N, as are Stockholm, Helsinki, and St. Petersburg; continue due east and you'll encounter Anchorage. Door latches suddenly give way. We might, for example, anchor bargeloads of evaporation-enhancing surfactants (used in the southwest corner of the Dead Sea to speed potash production) upwind from critical downwelling sites, letting winds spread them over the ocean surface all winter, just to ensure later flushing.

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An abrupt cooling could happen now, and the world might not warm up again for a long time: it looks as if the last warm period, having lasted 13, 000 years, came to an end with an abrupt, prolonged cooling. Then not only Europe but also, to everyone's surprise, the rest of the world gets chilled. Again, the difference between them amounts to nine to eighteen degrees—a range that may depend on how much ice there is to slow the responses. A meteor strike that killed most of the population in a month would not be as serious as an abrupt cooling that eventually killed just as many. But the ice ages aren't what they used to be. When the warm currents penetrate farther than usual into the northern seas, they help to melt the sea ice that is reflecting a lot of sunlight back into space, and so the earth becomes warmer. They even show the flips. Judging from the duration of the last warm period, we are probably near the end of the current one. This major change in ocean circulation, along with a climate that had already been slowly cooling for millions of years, led not only to ice accumulation most of the time but also to climatic instability, with flips every few thousand years or so. Glaciers pushing out into the ocean usually break off in chunks. The cold, dry winds blowing eastward off Canada evaporate the surface waters of the North Atlantic Current, and leave behind all their salt. Like a half-beaten cake mix, with strands of egg still visible, the ocean has a lot of blobs and streams within it. The system allows for large urban populations in the best of times, but not in the case of widespread disruptions.

It keeps northern Europe about nine to eighteen degrees warmer in the winter than comparable latitudes elsewhere—except when it fails. A nice little Amazon-sized waterfall flows over the ridge that connects Spain with Morocco, 800 feet below the surface of the strait. Natural disasters such as hurricanes and earthquakes are less troubling than abrupt coolings for two reasons: they're short (the recovery period starts the next day) and they're local or regional (unaffected citizens can help the overwhelmed). Five months after the ice dam at the Russell fjord formed, it broke, dumping a cubic mile of fresh water in only twenty-four hours. We must look at arriving sunlight and departing light and heat, not merely regional shifts on earth, to account for changes in the temperature balance. At the same time that the Labrador Sea gets a lessening of the strong winds that aid salt sinking, Europe gets particularly cold winters. But we can't assume that anything like this will counteract our longer-term flurry of carbon-dioxide emissions. Although I don't consider this scenario to be the most likely one, it is possible that solutions could turn out to be cheap and easy, and that another abrupt cooling isn't inevitable.

Those who will not reason. It then crossed the Atlantic and passed near the Shetland Islands around 1976. Greenland's east coast has a profusion of fjords between 70°N and 80°N, including one that is the world's biggest. When there has been a lot of evaporation, surface waters are saltier than usual. The return to ice-age temperatures lasted 1, 300 years. Pollen cores are still a primary means of seeing what regional climates were doing, even though they suffer from poorer resolution than ice cores (worms churn the sediment, obscuring records of all but the longest-lasting temperature changes). To keep a bistable system firmly in one state or the other, it should be kept away from the transition threshold. We are in a warm period now. By 1971-1972 the semi-salty blob was off Newfoundland. There is another part of the world with the same good soil, within the same latitudinal band, which we can use for a quick comparison. There is also a great deal of unsalted water in Greenland's glaciers, just uphill from the major salt sinks. But we may be able to do something to delay an abrupt cooling. Light switches abruptly change mode when nudged hard enough.

The better-organized countries would attempt to use their armies, before they fell apart entirely, to take over countries with significant remaining resources, driving out or starving their inhabitants if not using modern weapons to accomplish the same end: eliminating competitors for the remaining food. In discussing the ice ages there is a tendency to think of warm as good—and therefore of warming as better. By 125, 000 years ago Homo sapienshad evolved from our ancestor species—so the whiplash climate changes of the last ice age affected people much like us.