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Strategies & Market Trends : 2026 TeoTwawKi ... 2032 Darkest Interregnum -- Ignore unavailable to you. Want to Upgrade?

To: maceng2 who wrote (175583)	7/31/2021 5:57:56 AM
From: Haim R. Branisteanu	Respond to of 218910

Thank you

To: maceng2 who wrote (175583)	7/31/2021 6:23:05 AM
From: maceng2	2 Recommendations Recommended By isopatch Julius Wong Read Replies (1) \| Respond to of 218910

That link, in case anyone missed it. A Final Warning to Humanity from Former Pfizer Chief Scientist Michael Yeadon (bitchute.com)

To: maceng2 who wrote (175583)	7/31/2021 1:42:04 PM
From: Haim R. Branisteanu	Read Replies (2) \| Respond to of 218910

Open Access Published: 13 July 2021 #forestfires generating PyroCb smoke plumes reaching the lower stratosphere often result from multiple large wildfires in close proximity that produce several intense convective updrafts over a period of only a few hours. PyroCb intensity & ensuing stratospheric plume impacts, therefore, vary with the distribution & intensity of certain types of regional wildfire activity during periods that overlap with conditions that include conducive background meteorology. While regionally-focused pyroCb outbreaks deviate from single point sources associated with volcanic eruptions, the ensuing smoke plumes exhibit many similarities, traveling thousands of kilometers in both the upper troposphere and lower stratosphere, even encircling a portion of the globe. Smoke plumes ensuing from "Australian wildfires" (of 2019/20) reached extraordinary altitudes in the middle stratosphere (20–35?km), where the absorption of incoming sunlight by carbonaceous smoke particles can perturb radiative forcing & facilitate photochemical reactions that influence the ozone chemistry. The "Australian wildfires" also revealed that plumes injected by pyroCb activity can significantly alter the dynamic circulation in the lower stratosphere. This discovery raises many new questions on the scale and impact of pyroCb activity in the climate system at a time when stratospheric geoengineering is being evaluated as a response to climate change 32 and tropospheric smoke sources are often omitted from reviews of the lower-stratospheric aerosol system 33, 34.