Deep trough

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Deep trough

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Company Credits. Technical Specs. Plot Summary. Plot Keywords. Parents Guide. External Sites. User Reviews.

User Ratings. External Reviews. Metacritic Reviews. Photo Gallery. Trailers and Videos. Crazy Credits. Alternate Versions. Rate This. A woman with an unusual birth defect comes to a doctor who has an unorthodox solution to make the best of her situation.

Director: Gerard Damiano as Jerry Gerard. Writer: Gerard Damiano as Jerry Gerard. Added to Watchlist.

Sex, Censorship and the Silver Screen. Guide for the Film Fanatic by Danny Peary. I've watched a lot of movies!!!

Share this Rating Title: Deep Throat 5. Use the HTML below. You must be a registered user to use the IMDb rating plugin. Edit Cast Complete credited cast: Harry Reems Young Helen Wood Helen as Dolly Sharp Ronnie Shark Maltz as Bill Harrison William Love Wilber Wang Carol Connors The Nurse Bob Phillips Fenster Linda Lovelace Linda Lovelace Ted Street Delivery Boy John Byron Edit Storyline Linda, frustrated that her hugely energetic sex life leaves her unsatisfied, seeks medical help.

Taglines: How far does a girl have to go to untangle her tingle? Edit Did You Know? Trivia Star Linda Lovelace later distanced herself from the movie.

She claimed in her autobiography that Chuck Traynor, her then-husband, coerced her into participating. She said he would often persuade her to engage in sexual acts in front of the camera, and later prostituted her under threat of guns and violence.

Several people confirmed that Traynor was controlling and abusive on set; and Traynor himself admitted it.

A trough will usually begin with a positive tilt as cold air moves toward the Equator. Therefore, the clouds and precipitation will develop in the positive phase and the most severe weather will be in the negative phase.

In addition to standard troughs, some may be described further with a qualifying term indicating a specific or a set of characteristics.

An inverted trough is an atmospheric trough which is oriented opposite to most troughs of the mid-latitudes. Most but not all inverted troughs are tropical waves also commonly called easterly waves.

Most troughs of low pressure in the mid-latitudes of the Northern Hemisphere are characterized by decreasing atmospheric pressure from south to north while inverted troughs are characterized by decreasing pressure from north to south.

The situation is opposite in the Southern Hemisphere. Inverted troughs in both hemispheres move to the west from the east, while mid-latitude troughs generally move with the westerlies toward the east.

A lee trough, also known as a dynamic trough, is "A pressure trough formed on the lee side of a mountain range in situations where the wind is blowing with a substantial component across the mountain ridge; often seen on United States weather maps east of the Rocky Mountains, and sometimes east of the Appalachians, where it is less pronounced.

Convective cells may develop in the vicinity of troughs and give birth to a tropical cyclone. Some tropical or subtropical regions such as the Philippines or south China are greatly affected by convection cells along a trough.

In the mid-latitude westerlies , upper level troughs and ridges often alternate in a high-amplitude pattern. For a trough in the westerlies, the region just west of the trough axis is typically an area of convergent winds and descending air — and hence high pressure —, while the region just east of the trough axis is an area of fast, divergent winds and low pressure.

Tropical waves are a type of trough in easterly currents, a cyclonic northward deflection of the trade winds.

From Wikipedia, the free encyclopedia. Elongated region of low atmospheric pressure. A Dictionary of Geography. London: Edward Arnold Publishers Ltd.

Archived from the original on Retrieved Archived from the original on 12 March Retrieved 30 April National Weather Service.

Retrieved July 29, Glossary of Meteorology 2nd ed. American Meteorological Society. Archived from the original on 5 March Categories : Atmospheric dynamics Atmospheric circulation Synoptic meteorology and weather.

Hidden categories: Webarchive template wayback links CS1 maint: archived copy as title Articles with short description Short description matches Wikidata.

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Deep trough

Deep Trough Video

DEEP SLEEP music for Healing Insomnia - 1 hour Dream voyage Trough Sky and Clouds

A woman with an unusual birth defect comes to a doctor who has an unorthodox solution to make the best of her situation. Director: Gerard Damiano as Jerry Gerard.

Writer: Gerard Damiano as Jerry Gerard. Added to Watchlist. Sex, Censorship and the Silver Screen. Guide for the Film Fanatic by Danny Peary.

I've watched a lot of movies!!! Share this Rating Title: Deep Throat 5. Use the HTML below. You must be a registered user to use the IMDb rating plugin.

Edit Cast Complete credited cast: Harry Reems Young Helen Wood Helen as Dolly Sharp Ronnie Shark Maltz as Bill Harrison William Love Wilber Wang Carol Connors The Nurse Bob Phillips Fenster Linda Lovelace Linda Lovelace Ted Street Delivery Boy John Byron Edit Storyline Linda, frustrated that her hugely energetic sex life leaves her unsatisfied, seeks medical help.

Taglines: How far does a girl have to go to untangle her tingle? Edit Did You Know? Trivia Star Linda Lovelace later distanced herself from the movie.

She claimed in her autobiography that Chuck Traynor, her then-husband, coerced her into participating. She said he would often persuade her to engage in sexual acts in front of the camera, and later prostituted her under threat of guns and violence.

Several people confirmed that Traynor was controlling and abusive on set; and Traynor himself admitted it. Quotes Helen : Do you wanna get off or do you wanna wreck a city?

Alternate Versions Several openings to the film exist. The original opens with a text prologue referencing Freud and cuts to the familiar opening credits of Lovelace driving around Florida with the commonly known opening theme.

The Arrow home video version cuts this opening and begins with the first shot of Linda in the car. Another version of the opening starts with the car shot but with a completely different interlude in the background.

The Italian version retains the Freud opening with Italian text and has the opening titles, including Italian dubbing production credits, with the familiar opening music with Italian titles over still shots of Lovelace.

Was this review helpful to you? Yes No Report this. Add the first question. Language: English. Runtime: 61 min 50 min cut 85 min softcore.

Sound Mix: Mono. Color: Color Eastmancolor. Edit page. Clear your history. A trough is not in a general terms a boundary, but an elongated area of lower air pressure.

There are changes in wind direction across a trough but there is no change in air mass. While not specifically a surface boundary, troughs reflect the change in atmospheric conditions in the upper atmosphere.

As such, troughs can be areas where showers and thunderstorms can form. If a trough forms in the mid-latitudes, a temperature difference at some distance between the two sides of the trough usually exists and the trough might become a weather front at some point.

However such a weather front is usually less convective than a trough in the tropics or subtropics such as a tropical wave. Inversely, sometimes collapsed frontal systems will degenerate into troughs.

Sometimes the region between two high pressure centers may also assume the character of a trough when there is a detectable wind shift noted at the surface.

In the absence of a wind shift, the region is designated a col , akin to a geographic saddle between two mountain peaks. A trough is the result of the movements of the air in the atmosphere.

In regions where there is upward movement near the ground and divergence at altitude, there is a loss of mass. The pressure becomes lower at this point.

At upper levels of the atmosphere, this occurs when there is a meeting of a mass of cold air and another hot one along a thin ribbon called a frontal baroclinic zone.

We then have the creation of a jet stream that plunges the cold air towards the equator and hot air towards the poles, creating a ripple in the circulation that is called a Rossby wave.

In general, absolute vorticity advection is positive between these two features, but closer to the ridge, whereas it is negative just behind a trough.

At the surface, lifting air under positive vorticity advection is reflected by the formation of depressions and troughs. There will therefore be a slope between the barometric high altitude and that on the ground, this slope going towards the mass of cold air at high altitude generally towards the Pole.

Troughs have an orientation relative to the poles which is rarely North-South. In the Northern Hemisphere, positively tilted troughs will extend from the lowest pressure northeast to southwest while negatively tilted troughs have a northwest to southeast orientation.

A trough will usually begin with a positive tilt as cold air moves toward the Equator. Therefore, the clouds and precipitation will develop in the positive phase and the most severe weather will be in the negative phase.

In addition to standard troughs, some may be described further with a qualifying term indicating a specific or a set of characteristics.

An inverted trough is an atmospheric trough which is oriented opposite to most troughs of the mid-latitudes.

Most but not all inverted troughs are tropical waves also commonly called easterly waves. Most troughs of low pressure in the mid-latitudes of the Northern Hemisphere are characterized by decreasing atmospheric pressure from south to north while inverted troughs are characterized by decreasing pressure from north to south.

The situation is opposite in the Southern Hemisphere. Inverted troughs in both hemispheres move to the west from the east, while mid-latitude troughs generally move with the westerlies toward the east.

A lee trough, also known as a dynamic trough, is "A pressure trough formed on the lee side of a mountain range in situations where the wind is blowing with a substantial component across the mountain ridge; often seen on United States weather maps east of the Rocky Mountains, and sometimes east of the Appalachians, where it is less pronounced.

Convective cells may develop in the vicinity of troughs and give birth to a tropical cyclone. Some tropical or subtropical regions such as the Philippines or south China are greatly affected by convection cells along a trough.

Damas porno Learn to edit Community portal Recent changes Upload file. Therefore, the clouds and precipitation Aaliyah hadid age develop in the positive phase and the most Ffm homemade video weather will be in the negative phase. Maltz as Bill Harrison William Love Edit page. Official Sites.

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