Across The Pacific Full Movie
Oreo Huppe
Across the Pacific is a 1942 American spy film set on the eve of the entry of the United States into World War II. It was directed first by John Huston, then by Vincent Sherman after Huston joined the United States Army Signal Corps. It stars Humphrey Bogart, Mary Astor, and Sydney Greenstreet. Despite the title, the action never progresses across the Pacific, concluding in Panama. The original script portrayed an attempt to avert a Japanese plan to invade Pearl Harbor. When the real-life attack on Pearl Harbor occurred, production was shut down for three months, resuming on March 2, 1942, with a revised script changing the target to Panama.[4][5]
On November 17, 1941, on Governor's Island in New York City, Captain Rick Leland is court-martialed and discharged from the United States Army Coast Artillery Corps after he is caught stealing. He tries to join the Princess Patricia's Canadian Light Infantry but is coldly rebuffed. Ostensibly on his way to China to fight for Chiang Kai-shek, he boards a Japanese ship, the Genoa Maru, sailing from Halifax, Nova Scotia to Yokohama via the Panama Canal and Hawaii.
On board, he meets Canadian Alberta Marlow who claims to be from Medicine Hat, and a lighthearted romance begins. The other passengers are Dr. Lorenz and his servant, T. Oki. Lorenz, a professor of sociology, admires the Japanese and therefore is very unpopular in the Philippines, where he resides. Leland, in turn, makes it clear that he will fight for anyone willing to pay him enough.
During a stop in New York City, Leland is revealed as a secret agent when he reports to Colonel Hart, an undercover Army Intelligence officer. Lorenz is a known enemy spy, but Hart and Leland are uncertain about Marlow. Hart also warns him to look out for a Japanese criminal named Totsuiko. Returning to the ship, Leland surprises a Filipino assassin about to shoot Lorenz. Leland gains Lorenz's confidence by remaining indifferent when Lorenz has the man killed. Joe Totsuiko embarks as a passenger, in the guise of a wise-cracking young Nisei, and a different man returns as T. Oki. Lorenz pays Leland in advance for information concerning the military installations guarding the Panama Canal.
In Panama, the captain announces that Japanese ships are being denied entry into the Canal and must detour around Cape Horn. Leland, Marlow and Lorenz wait for another vessel at Sam's hotel. Crates addressed to Dan Morton, Bountiful Plantation, are unloaded. Lorenz demands that Leland procure up-to-date schedules for the air patrol. On December 6, 1941, Leland meets with his local contact, A. V. Smith, and convinces him to provide real timetables, as Lorenz would recognize fakes. Smith adds that plantation owner Dan Morton is a rich dipsomaniac and that Marlow is a buyer for Rogers Fifth Avenue in New York City.
Leland hands over the schedules and is brutally beaten. He revives several hours later and immediately calls Smith, warning him to change the patrol schedule. Smith is killed after Leland hangs up. Lorenz and Marlow are gone. Sam sends Leland to a cinema, where a man whispers, "Go Bountiful Plantation..." and is killed. At the plantation, Leland sees a torpedo bomber being prepared. He is captured and brought to Lorenz. Also present are Totsuiko, Marlow, Dan Morton, and the second T. Oki, who turns out to be a Japanese prince and pilot. Morton, whose weakness was exploited by the enemy agents to gain a base for their activities, is Marlow's father. Her only stake in the affair is his welfare.
Lorenz reveals that Smith is dead, so the prince can destroy the Panama Canal locks without interference. Totsuiko is left to guard the prisoners. When Morton staggers to his feet, Totsuiko shoots him, but that enables Leland to overpower Totsuiko. Outside, Leland seizes a machine gun, shoots down the bomber as it is taking off, and dispatches Lorenz's henchmen. In the house, a defeated Lorenz attempts to commit seppuku, but his nerve fails him. He begs Leland to kill him. Leland refuses, telling Lorenz he "has a date with Army Intelligence." Leland and Marlow clasp hands and look up at a sky filling with American planes.
After the hiatus caused by the attack on Pearl Harbor, production resumed on March 2, 1942, and filming continued through May 2, 1942 (including retakes). The film opened in New York City on September 4, 1942.[9]
Director John Huston was called up by the Army Service Forces Signal Corps during filming. In a later interview he claimed that he deliberately left Leland tied up and held at gunpoint in a cliff-hanger set up for his replacement to solve.[5] Vincent Sherman took over on April 22, 1942,[5] and finished directing the film (minus the script that Huston had taken with him, explaining "Bogie will know how to get out"). Afterwards, Huston declared that Sherman's solution to the problem "lacked credibility.[14] The studio's solution to the problem was to discard Huston's footage of the impossible dilemma and write a new scenario.[10]
A week after a heatwave broke records across the Southwest and northern Mountain West, a second, even more anomalous, heatwave occurred across the Pacific Northwest and Western Canada. It sent records toppling. Over a four-day period, June 26-29, daytime high temperatures skyrocketed to well over 100 degrees Fahrenheit, setting all-time records at dozens of locations.
As with most questions about the atmosphere, there are multiple answers. The most direct cause of the blistering heat was a high-pressure system, stronger than ever observed in the region, that sat over the region for several days, unwilling to move like a stubborn dog on a walk. The cloudless skies and sinking air associated with the high pressure helped record temperatures build.
In the future, according to the Climate Science Special report, the scientific basis for the fourth National Climate Assessment, heatwaves are projected to continue to get hotter, occur more often and last longer in the future due to the emissions of greenhouse gases.
Extreme heat this far north is particularly dangerous as these locations have a lot less experience with temperatures that high. Communities in the Southwest, for instance, have previous knowledge of temperatures over 100 degrees. Those in the Northwest and Canada simply do not. And this manifests itself through the built environment. Air conditioner use in the Southwest is virtually mandatory. Yet in Seattle, according to the New York Times, there is a culture against air conditioner use. NPR notes that Seattle ranked as the least air-conditioned city in a comparison of the top 15 metro areas in the U.S. Only 44% of homes in Seattle have primary air conditioning installed. Things are slightly better in Portland, at 78% of homes, but still far below the nationwide average.
Foam-core board covering the south-facing windows in the hallway of a Seattle home during the recent heatwave. Beyond the lack of air-conditioning, many homes have windows that are positioned and designed to maximize sun exposure. Photo by Dale Durran.
Episodic shifts in winds and water currents across the equatorial Pacific can cause floods in the South American desert while stalling and drying up the monsoon in Indonesia and India. Atmospheric circulation patterns that promote hurricanes and typhoons in the Pacific can also knock them down over the Atlantic. Fish populations in one part of the ocean might crash, while others thrive and spread well beyond their usual territory.
The circulation of the air above the tropical Pacific Ocean responds to this tremendous redistribution of ocean heat. The typically strong high-pressure systems of the eastern Pacific weaken, thus changing the balance of atmospheric pressure across the eastern, central, and western Pacific. While easterly winds tend to be dry and steady, Pacific westerlies tend to come in bursts of warmer, moister air.
El Nio usually alters the Pacific jet stream, stretching it eastward, making it more persistent, and bringing wetter conditions to the western U.S. and Mexico. (NASA Earth Observatory illustration by Joshua Stevens.)
What is not a mystery is that El Nio is one of the most important weather-producing phenomena on Earth, a "master weather-maker," as author Madeleine Nash once called it. The changing ocean conditions disrupt weather patterns and marine fisheries along the west coasts of the Americas. Dry regions of Peru, Chile, Mexico, and the southwestern United States are often deluged with rain and snow, and barren deserts have been known to explode in flowers. Meanwhile, wetter regions of the Brazilian Amazon and the northeastern United States often plunge into months-long droughts.
Typically dry regions can experience nearly two times as much rain during a strong El Nio. (NASA Earth Observatory chart by Joshua Stevens, using data from the California-Nevada Climate Applications Program.)
NASA, the National Oceanic and Atmospheric Administration (NOAA), and other scientific institutions track and study El Nio in many ways. From underwater floats that measure conditions in the depths of the Pacific to satellites that observe sea surface heights and the winds high above it, scientists now have many tools to dissect this l'enfant terrible of weather. The data visualizations on the next page show most of the key ways that we observe El Nio before, during, and after its visits.
The ocean is not uniform. Temperatures, salinity, and other characteristics vary in three dimensions, from north to south, east to west, and from the surface to the depths. With its own forms of underwater weather, the seas have fronts and circulation patterns that move heat and nutrients around ocean basins. Changes near the surface often start with changes in the depths.
The tropical Pacific receives more sunlight than any other region on Earth, and much of this energy is stored in the ocean as heat. Under neutral, normal conditions, the waters off southeast Asia and Australia are warmer and sea level stands higher than in the eastern Pacific; this warm water is pushed west and held there by easterly trade winds.
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