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Strategies & Market Trends : Taking Advantage of a Sharply Changing Environment

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Dec 19 9:30 AM EST

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Hawkmoon

To: teevee who wrote (2017)	9/7/2019 10:43:32 PM
From: Doug R	1 Recommendation of 6356

Not exactly current cloud cover data but it's a good overview of the net incoming/outgoing heat energy during certain times. dbirch214.wixsite.com During years of El Nino heat is retained and distributed poleward away from the Equator via "ocean Transport" and Walker circulation pattern, This effects the Amount of loss of irradience (OLR) Or outgoing Longwave Radiation, Net amount retained vs loss. Typically during June- September OHC during El Nino sees negative OLR indicative of enhanced convection and more cloud cover, More convective activity in the central and eastern equatorial Pacific implies higher , colder cloud tops, which emit much less infrared radiation into space, warmer terrestrial temperatures are greatest in the 0-70°N as this is the largest land mass. Moreover a loss in OHC at Equator would transpose in a greater loss of OLR to space and a loss of terrestrial temperature, given the SH winter this would reflect in a "plataue" or reduction in Global Temperatures. Below OLR graph since 2016.

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