Rain Slow Motion Video Download

Particle generators play an extremely important role in motion graphics. From rain to stars, particles have a way of adding in extra detail that will take your design to the next level, without having to keyframe or add movement to each shape. Did you know you can create particles in C4D without any third party plugins?

Even if you normally use After Effects to create rain this method is extremely helpful. Namely, because this method uses no 3rd party plug-ins. To get a similar looking effect in After Effects you would have to use a 3D particle generator like Trapcode Particular, which can be a bit costly.

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Well, researchers at the Massachusetts Institute of Technology believe they've discovered the source of the wonderful smell. The refreshing fragrance apparently comes from tiny bubbles of scented air that fizz up like champagne when a raindrop hits a porous surface.

New research also suggests that aerosols could also carry bacteria and viruses, Buie told ABC News. This could explain how diseases like E. coli might be transmitted to humans via rainfall and wind gusts, according to the video.

Australian scientists first studied and characterized this phenomenon using the word \"petrichor,\" which now means a smell that frequently accompanies the first rain after a period of warm, dry weather.

Florence markedly slowed down as it neared the N.C. coast. The day before landfall, the storm clocked 12 mph. The next morning, it chugged at 6 mph. By Saturday morning, the system crawled over land at a languid 2 mph.

Jacksonville, located on the New River in Onslow County, meanwhile saw a surge of more than 7 feet, according to a gauge owned by the N.C. Department of Public Safety. Another state gauge in Belhaven, on the Pungo River in Beaufort County, measured a surge surpassing 5.75 feet.

CHARLESTON, S.C. (CBS News) -- Historic rainfall levels were recorded in Charleston as the East Coast gets inundated in what has been called a slow-motion rain disaster as stormy weather settles in over the heavily populated region.

The National Weather Service reported 13 inches of rain, the greatest three-day rainfall total on record, have been recorded at the service's monitoring station at the Charleston International Airport, according to CBS affiliate WCSC in Charleston. The recorded daily rainfall total for Saturday was 11.5 inches of rain, setting a new one-day precipitation record for the airport.

The steady downpour drew its moisture from a slow-moving low-pressure system over the Southeast that has linked up to a finger of tropical moisture from Hurricane Joaquin. Heavy rain was expected to continue overnight in the Carolinas and parts of northern Georgia and could cause some significant river and stream flooding, the National Weather Service said.

Three people died in three separate weather-related traffic incidents in South Carolina since the heavy rains began, the state's highway patrol said, including two motorists who lost control of their cars and a pedestrian hit by a car.

Once the rain ends, the flood threat persists because the ground is too saturated to absorb water, meteorologists say. And high winds could topple trees like the one that hit a vehicle near Fayetteville, North Carolina, killing a passenger. The storm also has been linked to a drowning in Spartanburg, South Carolina.

Downtown Charleston was closed off to incoming traffic Saturday as rain flooded roads and left some motorists stranded as flood waters engulfed their cars, including a white BMW with water to the engine. At least two bridges were washed out in other parts of the state

In North Carolina, Agriculture Commissioner Steve Troxler says farmers are starting to see the impact of the continuous rain on their crops. Apples in Henderson County are starting to split open because they're waterlogged and farmers can't get into the fields to harvest other crops.

FIGURE 5. Feature constrained Zooming Slow-Mo network. Dynamic data use the situation from southeast of France as an example just for showing three kinds of dynamic data, and we used data from northwest of France in our experiment. Static data are the real data from northwest of France.

For the past couple of decades, I've held the belief that deer move more in the rain. Not heavy rain, mind you, but light to moderate precipitation. I can count the number of times I've sat in a treestand or ground blind, had little deer movement, and then they came out of the woodworks as the rain started falling from the sky.

I sat through a steady rain shower, and as it began to subside, deer poured out of the bedding area in front of me. First, a couple of nice 2-year-olds. Then a yearling buck. Then the giant velvet 8-pointer. Even more bucks, does, and fawns walked out afterward. They all fed out in the clover in front of me, all while it misted rain. Eventually, I got a shot opportunity and made it count.

That said, I think rain is more likely to get deer on their feet on warmer days, especially during the early season. Generally, rain cools you down, which gives deer reprieve from the heat, effectively getting them up on their feet.

I think rain showers that occur mid- to late-afternoon have even more power to get deer up and moving. When conditions align with crepuscular (dawn and dusk) movement, I believe it increases deer activity, even more than crepuscular movements without additional triggers.

Several colleges with teams dedicated to whitetail biology and behavior have attempted to address this question. While general whitetail behavior isn't the focus of most wildlife agencies and DNRs (they focus on resource management), even some of them have studied the impact of rain on whitetail movement.

Interestingly, some biologists and experts have discovered data or had experiences that suggest deer do, in fact, move more, if only slightly, during light to moderate rainfall. Both Boggess and Jaster have mixed feelings on the subject.

Boggess says that other researchers have found light rain can increase deer movement, but heavy rain can decrease it. Still, he says there is no consistent effect of rain across all the whitetail's range. That's a reasonable conclusion, though, mainly since whitetails inhabit a very diverse range of climates and habitats.

Boggess notes that rain softens twigs and leaves, which offers perfect stalking conditions. On rainy days, perhaps slowly still hunt and scout your way through deer habitat. Jaster says rain and wind likely make it more challenging to see hunters' movements, too. So, that's good.

But I think deer tend to move more during light rainfall, especially during the early season when temperatures are warmer and when the rain event occurs in the early morning or late afternoon. Perhaps only the deer I hunt like their salad with dressing, but I doubt that's true.

When eaten, Mushrooms slow down the in-game time by 50% & increase the player's mobility for about 20 seconds, which is visually shown as the Slugcat shaking, blinking much faster, and emitting waves that distort the surrounding pixels.

These effects have a variety of applications in combat - they can make it easier to avoid getting grabbed, hit certain creatures' weak spots, or get away if needed.

The increased running speed and jump height can also allow the Slugcat to make it past some otherwise impassable gaps, and generally make traversing the world more efficient, while the slow motion effect may come in handy for catching nimble prey, like Batflies or Eggbugs.

The amount of rainfall a tropical storm or hurricane can produce is a function of its forward speed. As illustrated in the graphic below, the slower the speed, the more incredible the rainfall amounts can become.

A storm chugging along at just 5 mph has a rainfall potential upwards of 30 inches, while one moving briskly at 20 mph typically produces much smaller rain totals in any given location. When this occurs near mountainous terrain, rainfall totals can be further enhanced.

Hurricane Harvey is the most extreme example of the major flooding caused by a storm that stalls out or moves slowly. Catastrophic damage occurred in Houston and other parts of southeastern Texas after Harvey spent days soaking the state.

In 1994, flooding from Tropical Storm Alberto killed 31 people as it moved slowly across the western Florida Panhandle, Alabama and Georgia. Americus, Georgia, received 21 inches of rain in just 24 hours.

Making matters worse is the heavy rain from slow storms quickly saturating soil conditions. The persistent winds in combination with the soaked soil can make trees topple easier at lower wind speeds than otherwise with drier soil.

One of the most recent examples was Hurricane Isaac in 2012, which moved slowly and stalled at one point near the Louisiana coast. Though Isaac's maximum strength was a Category 1, its large wind field and slow movement prolonged the storm-surge inundation.

To validate this hypothesis, we must eliminate the possibility that the rain alone could have generated equivalent landslide displacements during the 2016 wet season. To do so, we focused our attention on the 2014 and 2017 rainy seasons and the displacements observed over these periods.

Almost immediately after earthquake shaking, the dv/v was seen to recover. This recovery was clearly visible, for instance, with the August 2016 earthquake (Fig. 2c and Supplementary Fig. 3f). This healing phase can be interpreted as the re-compaction of the soil as fractures close, and the grains cement together, reflecting a viscoelastic response of the soil47,48,50,51,52. This slow healing was also observed at laboratory-scale, where it is referred to as slow dynamics53. Previous observations of the dv/v recovery after an earthquake show that it often evolves logarithmically over time47,48,51. A similar pattern was also observed here, with recovery of the pre-earthquake soil state around one and a half months after the Ml 5.5 earthquake in August 2016 (Fig. 2c, light-green logarithmic curve and Supplementary Fig. 3f). However, recovery is questionable during the wet season, as we cannot separate it from the drainage process. This becomes even more complicated when small-earthquake activity is high, as we will see in the next sections. e24fc04721