Spike Jonze and Lance Bangs directed portrait of author of "Where the Wild Things Are"
'2012' Director Grilled on 3D and Destruction Movies
"It’s like I created the genre myself and I'm a prisoner to it."
Getty Images
Back in 1977, German-born Roland Emmerich enrolled in the Munich University of Film and Television to be a production designer. Later that year, he saw “Star Wars” and decided to switch to the director program. More than three decades later, that decision proved to be a prudent one. Known for his disaster films, Emmerich has directed one of the highest grossing films of all time, “Independence Day,” and several others that have topped the $100 million mark, such as “The Patriot,” “The Day After Tomorrow” and “Godzilla.”
His upcoming “2012” -- previewed at Comic-Con and due out Nov. 13 -- is yet another disaster flick. Inspired by the Mayan prophecy of a doomsday event in the winter of 2012 -- and starring John Cusack, Woody Harrelson and Danny Glover -- it's about a global catastrophe that leads to the end of the world.
How is it that you’ve made so many disaster movies? What do you think of all day?
In essence, I'm a very positive person. But deep down I'm very afraid. I'm afraid of everything. So it's just one of these things where it's interesting sometimes when you, as an artist, just dream up things and then all of a sudden everybody around you says, “How did you know that.” I said, “Don't ask me. I just felt it, you know?”
Does it get challenging trying to destroy the world in unique ways?
I don't know. That's my speciality. I think it started with "Independence Day." And I tell you it’s like I created the genre myself and I'm a prisoner to it.
I have to say this -- I've announced this so I can never ever go back -- "2012" will be my last disaster movie. At one point during the process of coming up with the story, I all of a sudden wavered. Right ... I wavered! And I said, “Harald [Kloser, his composer and co-writer on "2012," among other projects], I cannot do another destruction movie. This is like way too much destruction.” And he said, “But, Roland, you can now have the technology which is out there and make the model for a disaster movie. Do you want to have somebody else make that?” I said, “Okay, I’ll do it.”
And then I really redid the model of all disaster movies, trust me. When people see it they will say, “Oh my gosh.” I wanted to say the "F" word, but I didn't.
What role does technology play for you as a filmmaker?
Well a big one [laughs]. I'm sitting every day for two or three hours in the visual effects review [laughs again]. I actually love the possibilities you have these days to get the images which are in your head on film. We are at a stage where you can pretty much do everything if you have the money and the time.
How fast has the technology evolved since "Independence Day"?
Volker Engel -- who was the visual effects supervisor on "Independence Day" and is also doing "2012" -- and I always talk about how much has changed and how great it would have been if we had this technology at that time.



Comments
mack10 Says
Greenhouse gases
Main articles: Greenhouse gas and Greenhouse effect
Greenhouse effect schematic showing energy flows between space, the atmosphere, and earth's surface. Energy exchanges are expressed in watts per square meter (W/m2).
Recent atmospheric carbon dioxide (CO2) increases. Monthly CO2 measurements display seasonal oscillations in overall yearly uptrend; each year's maximum occurs during the Northern Hemisphere's late spring, and declines during its growing season as plants remove some atmospheric CO2.The greenhouse effect is the process by which absorption and emission of infrared radiation by gases in the atmosphere warm a planet's lower atmosphere and surface. It was discovered by Joseph Fourier in 1824 and was first investigated quantitatively by Svante Arrhenius in 1896.[19] Existence of the greenhouse effect as such is not disputed, even by those who do not agree that the recent temperature increase is attributable to human activity. The question is instead how the strength of the greenhouse effect changes when human activity increases the concentrations of greenhouse gases in the atmosphere.
Naturally occurring greenhouse gases have a mean warming effect of about 33 °C (59 °F).[20][C] The major greenhouse gases are water vapor, which causes about 36–70 percent of the greenhouse effect; carbon dioxide (CO2), which causes 9–26 percent; methane (CH4), which causes 4–9 percent[not in citation given]; and ozone (O3), which causes 3–7 percent.[21][22] Clouds also affect the radiation balance, but they are composed of liquid water or ice and so are considered separately from water vapor and other gases.
Human activity since the Industrial Revolution has increased the amount of greenhouse gases in the atmosphere, leading to increased radiative forcing from CO2, methane, tropospheric ozone, CFCs and nitrous oxide. The concentrations of CO2 and methane have increased by 36% and 148% respectively since the mid-1700s.[23] These levels are much higher than at any time during the last 650,000 years, the period for which reliable data has been extracted from ice cores.[24] Less direct geological evidence indicates that CO2 values this high were last seen about 20 million years ago.[25] Fossil fuel burning has produced about three-quarters of the increase in CO2 from human activity over the past 20 years. Most of the rest is due to land-use change, particularly deforestation.[26]
CO2 concentrations are continuing to rise due to burning of fossil fuels and land-use change. The future rate of rise will depend on uncertain economic, sociological, technological, and natural developments. Accordingly, the IPCC Special Report on Emissions Scenarios gives a wide range of future CO2 scenarios, ranging from 541 to 970 ppm by the year 2100.[27] Fossil fuel reserves are sufficient to reach these levels and continue emissions past 2100 if coal, tar sands or methane clathrates are extensively exploited.[28]
The destruction of stratospheric ozone by chlorofluorocarbons is sometimes mentioned in relation to global warming. mp3 indir usdown.net watchfootballlive.org watchnflfootballlive.net watchfootballlive.org nflfootballonline.org nflfootballonline.net nflfootballlive.net Although there are a few areas of linkage, the relationship between the two is not strong. Reduction of stratospheric ozone has a cooling influence, but substantial ozone depletion did not occur until the late 1970s.[29] Tropospheric ozone contributes to surface warming
mack10 Says
Greenhouse gases
Main articles: Greenhouse gas and Greenhouse effect
Greenhouse effect schematic showing energy flows between space, the atmosphere, and earth's surface. Energy exchanges are expressed in watts per square meter (W/m2).
Recent atmospheric carbon dioxide (CO2) increases. Monthly CO2 measurements display seasonal oscillations in overall yearly uptrend; each year's maximum occurs during the Northern Hemisphere's late spring, and declines during its growing season as plants remove some atmospheric CO2.The greenhouse effect is the process by which absorption and emission of infrared radiation by gases in the atmosphere warm a planet's lower atmosphere and surface. It was discovered by Joseph Fourier in 1824 and was first investigated quantitatively by Svante Arrhenius in 1896.[19] Existence of the greenhouse effect as such is not disputed, even by those who do not agree that the recent temperature increase is attributable to human activity. The question is instead how the strength of the greenhouse effect changes when human activity increases the concentrations of greenhouse gases in the atmosphere.
Naturally occurring greenhouse gases have a mean warming effect of about 33 °C (59 °F).[20][C] The major greenhouse gases are water vapor, which causes about 36–70 percent of the greenhouse effect; carbon dioxide (CO2), which causes 9–26 percent; methane (CH4), which causes 4–9 percent[not in citation given]; and ozone (O3), which causes 3–7 percent.[21][22] Clouds also affect the radiation balance, but they are composed of liquid water or ice and so are considered separately from water vapor and other gases.
Human activity since the Industrial Revolution has increased the amount of greenhouse gases in the atmosphere, leading to increased radiative forcing from CO2, methane, tropospheric ozone, CFCs and nitrous oxide. The concentrations of CO2 and methane have increased by 36% and 148% respectively since the mid-1700s.[23] These levels are much higher than at any time during the last 650,000 years, the period for which reliable data has been extracted from ice cores.[24] Less direct geological evidence indicates that CO2 values this high were last seen about 20 million years ago.[25] Fossil fuel burning has produced about three-quarters of the increase in CO2 from human activity over the past 20 years. Most of the rest is due to land-use change, particularly deforestation.[26]
CO2 concentrations are continuing to rise due to burning of fossil fuels and land-use change. The future rate of rise will depend on uncertain economic, sociological, technological, and natural developments. Accordingly, the IPCC Special Report on Emissions Scenarios gives a wide range of future CO2 scenarios, ranging from 541 to 970 ppm by the year 2100.[27] Fossil fuel reserves are sufficient to reach these levels and continue emissions past 2100 if coal, tar sands or methane clathrates are extensively exploited.[28]
The destruction of stratospheric ozone by chlorofluorocarbons is sometimes mentioned in relation to global warming. mp3 indir usdown.net watchfootballlive.org watchnflfootballlive.net watchfootballlive.org nflfootballonline.org nflfootballonline.net nflfootballlive.net Although there are a few areas of linkage, the relationship between the two is not strong. Reduction of stratospheric ozone has a cooling influence, but substantial ozone depletion did not occur until the late 1970s.[29] Tropospheric ozone contributes to surface warming
mack10 Says
Greenhouse gases
Main articles: Greenhouse gas and Greenhouse effect
Greenhouse effect schematic showing energy flows between space, the atmosphere, and earth's surface. Energy exchanges are expressed in watts per square meter (W/m2).
Recent atmospheric carbon dioxide (CO2) increases. Monthly CO2 measurements display seasonal oscillations in overall yearly uptrend; each year's maximum occurs during the Northern Hemisphere's late spring, and declines during its growing season as plants remove some atmospheric CO2.The greenhouse effect is the process by which absorption and emission of infrared radiation by gases in the atmosphere warm a planet's lower atmosphere and surface. It was discovered by Joseph Fourier in 1824 and was first investigated quantitatively by Svante Arrhenius in 1896.[19] Existence of the greenhouse effect as such is not disputed, even by those who do not agree that the recent temperature increase is attributable to human activity. The question is instead how the strength of the greenhouse effect changes when human activity increases the concentrations of greenhouse gases in the atmosphere.
Naturally occurring greenhouse gases have a mean warming effect of about 33 °C (59 °F).[20][C] The major greenhouse gases are water vapor, which causes about 36–70 percent of the greenhouse effect; carbon dioxide (CO2), which causes 9–26 percent; methane (CH4), which causes 4–9 percent[not in citation given]; and ozone (O3), which causes 3–7 percent.[21][22] Clouds also affect the radiation balance, but they are composed of liquid water or ice and so are considered separately from water vapor and other gases.
Human activity since the Industrial Revolution has increased the amount of greenhouse gases in the atmosphere, leading to increased radiative forcing from CO2, methane, tropospheric ozone, CFCs and nitrous oxide. The concentrations of CO2 and methane have increased by 36% and 148% respectively since the mid-1700s.[23] These levels are much higher than at any time during the last 650,000 years, the period for which reliable data has been extracted from ice cores.[24] Less direct geological evidence indicates that CO2 values this high were last seen about 20 million years ago.[25] Fossil fuel burning has produced about three-quarters of the increase in CO2 from human activity over the past 20 years. Most of the rest is due to land-use change, particularly deforestation.[26]
CO2 concentrations are continuing to rise due to burning of fossil fuels and land-use change. The future rate of rise will depend on uncertain economic, sociological, technological, and natural developments. Accordingly, the IPCC Special Report on Emissions Scenarios gives a wide range of future CO2 scenarios, ranging from 541 to 970 ppm by the year 2100.[27] Fossil fuel reserves are sufficient to reach these levels and continue emissions past 2100 if coal, tar sands or methane clathrates are extensively exploited.[28]
The destruction of stratospheric ozone by chlorofluorocarbons is sometimes mentioned in relation to global warming. mp3 indir usdown.net watchfootballlive.org watchnflfootballlive.net watchfootballlive.org nflfootballonline.org nflfootballonline.net nflfootballlive.net Although there are a few areas of linkage, the relationship between the two is not strong. Reduction of stratospheric ozone has a cooling influence, but substantial ozone depletion did not occur until the late 1970s.[29] Tropospheric ozone contributes to surface warming
mack10 Says
Greenhouse gases
Main articles: Greenhouse gas and Greenhouse effect
Greenhouse effect schematic showing energy flows between space, the atmosphere, and earth's surface. Energy exchanges are expressed in watts per square meter (W/m2).
Recent atmospheric carbon dioxide (CO2) increases. Monthly CO2 measurements display seasonal oscillations in overall yearly uptrend; each year's maximum occurs during the Northern Hemisphere's late spring, and declines during its growing season as plants remove some atmospheric CO2.The greenhouse effect is the process by which absorption and emission of infrared radiation by gases in the atmosphere warm a planet's lower atmosphere and surface. It was discovered by Joseph Fourier in 1824 and was first investigated quantitatively by Svante Arrhenius in 1896.[19] Existence of the greenhouse effect as such is not disputed, even by those who do not agree that the recent temperature increase is attributable to human activity. The question is instead how the strength of the greenhouse effect changes when human activity increases the concentrations of greenhouse gases in the atmosphere.
Naturally occurring greenhouse gases have a mean warming effect of about 33 °C (59 °F).[20][C] The major greenhouse gases are water vapor, which causes about 36–70 percent of the greenhouse effect; carbon dioxide (CO2), which causes 9–26 percent; methane (CH4), which causes 4–9 percent[not in citation given]; and ozone (O3), which causes 3–7 percent.[21][22] Clouds also affect the radiation balance, but they are composed of liquid water or ice and so are considered separately from water vapor and other gases.
Human activity since the Industrial Revolution has increased the amount of greenhouse gases in the atmosphere, leading to increased radiative forcing from CO2, methane, tropospheric ozone, CFCs and nitrous oxide. The concentrations of CO2 and methane have increased by 36% and 148% respectively since the mid-1700s.[23] These levels are much higher than at any time during the last 650,000 years, the period for which reliable data has been extracted from ice cores.[24] Less direct geological evidence indicates that CO2 values this high were last seen about 20 million years ago.[25] Fossil fuel burning has produced about three-quarters of the increase in CO2 from human activity over the past 20 years. Most of the rest is due to land-use change, particularly deforestation.[26]
CO2 concentrations are continuing to rise due to burning of fossil fuels and land-use change. The future rate of rise will depend on uncertain economic, sociological, technological, and natural developments. Accordingly, the IPCC Special Report on Emissions Scenarios gives a wide range of future CO2 scenarios, ranging from 541 to 970 ppm by the year 2100.[27] Fossil fuel reserves are sufficient to reach these levels and continue emissions past 2100 if coal, tar sands or methane clathrates are extensively exploited.[28]
The destruction of stratospheric ozone by chlorofluorocarbons is sometimes mentioned in relation to global warming. mp3 indir usdown.net watchfootballlive.org watchnflfootballlive.net watchfootballlive.org nflfootballonline.org nflfootballonline.net nflfootballlive.net Although there are a few areas of linkage, the relationship between the two is not strong. Reduction of stratospheric ozone has a cooling influence, but substantial ozone depletion did not occur until the late 1970s.[29] Tropospheric ozone contributes to surface warming
xray19 Says
And then I really redid the model of all disaster movies, trust me. When people see it they will say, “Oh my gosh.” I wanted to say the "F" word, but I didn't.free games
pera Says
Oh, Emmerich is going science now? Burning fireballs from volcanic eruption seen in the trailer? Hollywood-science, Roland, not science. And pathetic Hollywood-scientists, not real-type scientists.