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#1
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Someone tell me how a warm pool in the south Pacific can affect the
north Indian without the ability to cross the equator. We are talking about a temperature difference here of something less than a degree Centigrade: From Earth Observatory: La Niņa, the counterpart to El Niņo, alters rainfall patterns over the Pacific and Indian Ocean basins. La Niņa develops when stronger-than-average trade winds push the warm surface waters of the equatorial Pacific west. Since cold water rises to replace the warm water, La Niņa leaves the eastern and central Pacific Ocean much cooler than normal, while the western Pacific is much warmer than normal. These anomalies in sea surface temperature are mirrored in rainfall patterns, with warmer-than-normal temperatures resulting in enhanced rainfall. In general, La Niņa brings unusually heavy rain to the West Pacific, Indonesia, parts of South east Asia, and northern Australia. http://earthobservatory.nasa.gov/New...3?img_id=17901 |
#2
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I see a reference to the equatorial Pacific, not exclusively the
southern hemispheric Pacific. On Jan 22, 10:14 pm, Weatherlawyer wrote: Someone tell me how a warm pool in the south Pacific can affect the north Indian without the ability to cross the equator. We are talking about a temperature difference here of something less than a degree Centigrade: From Earth Observatory: La Niņa, the counterpart to El Niņo, alters rainfall patterns over the Pacific and Indian Ocean basins. La Niņa develops when stronger-than-average trade winds push the warm surface waters of the equatorial Pacific west. Since cold water rises to replace the warm water, La Niņa leaves the eastern and central Pacific Ocean much cooler than normal, while the western Pacific is much warmer than normal. These anomalies in sea surface temperature are mirrored in rainfall patterns, with warmer-than-normal temperatures resulting in enhanced rainfall. In general, La Niņa brings unusually heavy rain to the West Pacific, Indonesia, parts of South east Asia, and northern Australia. http://earthobservatory.nasa.gov/New...ges.php3?img_i... |
#3
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Weatherlawyer wrote:
Someone tell me how a warm pool in the south Pacific can affect the north Indian without the ability to cross the equator. We are talking about a temperature difference here of something less than a degree Centigrade: From Earth Observatory: La Niņa, the counterpart to El Niņo, alters rainfall patterns over the Pacific and Indian Ocean basins. La Niņa develops when stronger-than-average trade winds push the warm surface waters of the equatorial Pacific west. Since cold water rises to replace the warm water, La Niņa leaves the eastern and central Pacific Ocean much cooler than normal, while the western Pacific is much warmer than normal. These anomalies in sea surface temperature are mirrored in rainfall patterns, with warmer-than-normal temperatures resulting in enhanced rainfall. In general, La Niņa brings unusually heavy rain to the West Pacific, Indonesia, parts of South east Asia, and northern Australia. http://earthobservatory.nasa.gov/New...3?img_id=17901 Please note the near-surface current that flows from the N. Pacific, across Indonesia, into the Indian Ocean. http://en.wikipedia.org/wiki/Thermohaline_circulation |
#4
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On Jan 23, 2:12 pm, David wrote:
Weatherlawyer wrote: Someone tell me how a warm pool in the south Pacific can affect the north Indian without the ability to cross the equator. We are talking about a temperature difference here of something less than a degree Centigrade: From Earth Observatory: La Niņa, the counterpart to El Niņo, alters rainfall patterns over the Pacific and Indian Ocean basins. La Niņa develops when stronger-than-average trade winds push the warm surface waters of the equatorial Pacific west. Since cold water rises to replace the warm water, La Niņa leaves the eastern and central Pacific Ocean much cooler than normal, while the western Pacific is much warmer than normal. These anomalies in sea surface temperature are mirrored in rainfall patterns, with warmer-than-normal temperatures resulting in enhanced rainfall. In general, La Niņa brings unusually heavy rain to the West Pacific, Indonesia, parts of South east Asia, and northern Australia. http://earthobservatory.nasa.gov/New...ges.php3?img_i.... Please note the near-surface current that flows from the N. Pacific, across Indonesia, into the Indian Ocean. http://en.wikipedia.org/wiki/Thermohaline_circulation Please note how near Peru this convective current gets. Venezuela. What is that recalcitrant scion of democracy up to there I wonder. I doubt he has much influence on a certain moneycrazy. No matter what its chimp says. Whatever the case the fact remains that the temperature difference is only a fraction of one degree centigrade. It is customary to link weather events in either hemisphere with the currents of the surface water over which they flow. Rightly or wrongly any egress of the Peruvian current across the equatorial counter current leaves a lot to be desired in reference to its effect on massive weather systems in the northern hemisphere. Their root causes however, are a completely different thing. And of course one of us has the answer to that. Or not, as the case may be. |
#5
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On Tue, 22 Jan 2008 20:14:17 -0800 (PST),
Weatherlawyer , in wrote: + Someone tell me how a warm pool in the south Pacific can affect the + north Indian without the ability to cross the equator. Well, actually the warm pool exists on both sides of the equator. + La Niņa develops when stronger-than-average trade winds push the warm + surface waters of the equatorial Pacific west. Since cold water rises + to replace the warm water, La Niņa leaves the eastern and central + Pacific Ocean much cooler than normal, while the western Pacific is + much warmer than normal. + + These anomalies in sea surface temperature are mirrored in rainfall + patterns, with warmer-than-normal temperatures resulting in enhanced + rainfall. In general, La Niņa brings unusually heavy rain to the West + Pacific, Indonesia, parts of South east Asia, and northern Australia. So, for both La Niņa and El Niņo the warm pool is offset from an "average" position. During El Niņo, it shifts to the east so that it's closer to the western hemisphere. And during La Niņa, it shifts to the west, so that it's closer to Asia/Northwest Australia. And the convective thunderstorms develop over the warm pool. In turn, they act to anchor the subtropical jetstream, which changes its position in the mid-latitudes, and thus influences the larger weather pattern. So, during La Niņa you get more rain in Manila than you would expect, and less over Peru. And during El Niņo, you get more rain in Peru than you would expect, and less in Manilla. -- Consulting Minister for Consultants, DNRC I can please only one person per day. Today is not your day. Tomorrow isn't looking good, either. I am BOFH. Resistance is futile. Your network will be assimilated. |
#6
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On Jan 23, 9:13 pm, I R A Darth Aggie wrote:
So, for both La Niņa and El Niņo the warm pool is offset from an "average" position. During El Niņo, it shifts to the east so that it's closer to the western hemisphere. And during La Niņa, it shifts to the west, so that it's closer to Asia/Northwest Australia. And the convective thunderstorms develop over the warm pool. In turn, they act to anchor the subtropical jet-stream, which changes its position in the mid-latitudes, and thus influences the larger weather pattern. So, during La Niņa you get more rain in Manila than you would expect, and less over Peru. And during El Niņo, you get more rain in Peru than you would expect, and less in Manilla. If only things were that simple. They may work like that on your computer networks but the earth is an analogue machine and subject to different vagaries. But if the world works according to Aggian principles, what you have described is a change in orders of magnitude from a a slightly warmer pool to a stream of low pressure, high altitude air. All through the power of a thunderstorm. No offence but you should get a job vetting scripts for Star Trek. |
#7
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Weatherlawyer wrote:
On Jan 23, 2:12 pm, David wrote: Weatherlawyer wrote: Someone tell me how a warm pool in the south Pacific can affect the north Indian without the ability to cross the equator. We are talking about a temperature difference here of something less than a degree Centigrade: From Earth Observatory: La Niņa, the counterpart to El Niņo, alters rainfall patterns over the Pacific and Indian Ocean basins. La Niņa develops when stronger-than-average trade winds push the warm surface waters of the equatorial Pacific west. Since cold water rises to replace the warm water, La Niņa leaves the eastern and central Pacific Ocean much cooler than normal, while the western Pacific is much warmer than normal. These anomalies in sea surface temperature are mirrored in rainfall patterns, with warmer-than-normal temperatures resulting in enhanced rainfall. In general, La Niņa brings unusually heavy rain to the West Pacific, Indonesia, parts of South east Asia, and northern Australia. http://earthobservatory.nasa.gov/New...ges.php3?img_i... Please note the near-surface current that flows from the N. Pacific, across Indonesia, into the Indian Ocean. http://en.wikipedia.org/wiki/Thermohaline_circulation Please note how near Peru this convective current gets. Venezuela. What is that recalcitrant scion of democracy up to there I wonder. I doubt he has much influence on a certain moneycrazy. No matter what its chimp says. Whatever the case the fact remains that the temperature difference is only a fraction of one degree centigrade. It is customary to link weather events in either hemisphere with the currents of the surface water over which they flow. Rightly or wrongly any egress of the Peruvian current across the equatorial counter current leaves a lot to be desired in reference to its effect on massive weather systems in the northern hemisphere. Their root causes however, are a completely different thing. And of course one of us has the answer to that. Or not, as the case may be. What is the volume of the troposphere? How much energy is required to raise the temperature of that much gas 0.5 degrees C? |
#8
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On Jan 24, 2:59 am, David wrote:
Rightly or wrongly any egress of the Peruvian current across the equatorial counter current leaves a lot to be desired in reference to its effect on massive weather systems in the northern hemisphere. Their root causes however, are a completely different thing. And of course one of us has the answer to that. Or not, as the case may be. What is the volume of the troposphere? How much energy is required to raise the temperature of that much gas 0.5 degrees C? La Nina is a cold spot. I forgot. Sorry. Which begs another question for another poster here who mooted its connection to thunderstorms. Do equatorial water breed thunderstorms? Anyone? By the by, am I the only one here who thinks the original premise is codswallop? I must have missed out on all that careful conditioning that seems to have had such a persuasive effect on the rest of you. Still, never mind eh? I'm here now. Let's see if I can fire up another brain cell. ****. I thought I had a spare. It turned out to be ear wax. Anyway, whilst I still have some resonance in the one I am using: If low pressure areas are warm pressure areas... no that's not right. Seeing as warm water imbues the cyclonic spells with.. hmm... that's a tricky one. Anticyclones are the warm ones aren't they... I think I had best quit this thing. |
#9
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On Wed, 23 Jan 2008 13:34:47 -0800 (PST),
Weatherlawyer , in wrote: + On Jan 23, 9:13 pm, I R A Darth Aggie wrote: + If only things were that simple. They may work like that on your + computer networks but the earth is an analogue machine and subject to + different vagaries. Yeah, no. That's the *observed* behaviour. + But if the world works according to Aggian principles, what you have + described is a change in orders of magnitude from a a slightly warmer + pool to a stream of low pressure, high altitude air. + + All through the power of a thunderstorm. + No offence but you should get a job vetting scripts for Star Trek. Maybe you should take some meteorology courses? no, that would be too much like, I dunno, logical or something. -- Consulting Minister for Consultants, DNRC I can please only one person per day. Today is not your day. Tomorrow isn't looking good, either. I am BOFH. Resistance is futile. Your network will be assimilated. |
#10
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On Wed, 23 Jan 2008 20:41:41 -0800 (PST),
Weatherlawyer , in wrote: + Which begs another question for another poster here who mooted its + connection to thunderstorms. Do equatorial water breed thunderstorms? + Anyone? Why don't you go look at satellite images, then overlay that with oceanography charts showing areas of upwelling (cold surface water) and downwelling (warm surface water)? Think you'll find a correlation? if that's a "yes", the question becomes "what is the cause of this correlation?" -- Consulting Minister for Consultants, DNRC I can please only one person per day. Today is not your day. Tomorrow isn't looking good, either. I am BOFH. Resistance is futile. Your network will be assimilated. |
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