THE NEW CLIMATE of NORDIC JUNGLE.
LARGE SCALE SUBSIDENCE.
by Henryk Szubinski
The tropics in Scandinavia.
date 2018
June 5
Some days ago after the tropical day in Scandinavia there appeared the Cirrus
clouds that are higher up in the layer between the Stratosphere and the troposphere.
The reasons being that the humidity created goes back up to the later between the stratosphere and the troposphere , inputting the valuable water needed for this layer of the atmosphere so that the balance is symbiotic, meaning it does not evaporate. However because this is vital for Earth's water balance these clouds evaporate where they are in a matter of minutes.
Here's the report from:
www.thelocal.se/20180603/sweden-sees-earliest-tropical-night-since-1950
date 2018
June 5
time, 16:01
Sweden on Saturday registered its earliest ‘tropical night’ in close to 70 years, as the record warmth seen in May carries on into June.
The lowest temperature on Saturday night on the island of Vinga near Gothenburg was 20.1C, qualifying the night for ‘tropical’ status, defined as a 24-hour period where the temperature never drops below 20C.
“It’s extremely unusual that we have a tropical night before the middle of June,” Alexandra Ohlsson, meteorologist on duty at Sweden’s SMHI weather forecaster, told Sweden's TT newswire.
In the 68 years since 1950, there has only been one year, 1986, when a tropical night has been recorded similarly early, in Kullen, also on Sweden’s West coast -- but that was two days later on June 4.
Last year, there was no tropical night at all, in 2016 it came on July 24, and in 2015 on July 2.
SMHI tweeted the news of the unusually early warmth.
from:
www.sunsail.com.au/blog/know-your-clouds
date 2018
June 5
time, 15:34
high level clouds
Cirrus clouds
So you’re sailing along under clear blue skies. You glance to port, and see no clouds; you swivel to starboard, nada. Then, you look over the bow once more, and in the far distance you see long, wispy streaks of cloud high in the sky. These, my friend, are Cirrus clouds, sometimes known as mare‘s tails.
Though they won’t leak on you, they indicate the arrival of a potentially wet warm front, so take note of their speed and direction. If they are heading to the east, you’re in luck, and fair weather is on its way. If not, you may be in for some rain and strong wind before things brighten up.
LARGE SCALE SUBSIDENCE.
by Henryk Szubinski
The tropics in Scandinavia.
date 2018
June 5
Some days ago after the tropical day in Scandinavia there appeared the Cirrus
clouds that are higher up in the layer between the Stratosphere and the troposphere.
The reasons being that the humidity created goes back up to the later between the stratosphere and the troposphere , inputting the valuable water needed for this layer of the atmosphere so that the balance is symbiotic, meaning it does not evaporate. However because this is vital for Earth's water balance these clouds evaporate where they are in a matter of minutes.
Here's the report from:
www.thelocal.se/20180603/sweden-sees-earliest-tropical-night-since-1950
date 2018
June 5
time, 16:01
Sweden on Saturday registered its earliest ‘tropical night’ in close to 70 years, as the record warmth seen in May carries on into June.
The lowest temperature on Saturday night on the island of Vinga near Gothenburg was 20.1C, qualifying the night for ‘tropical’ status, defined as a 24-hour period where the temperature never drops below 20C.
“It’s extremely unusual that we have a tropical night before the middle of June,” Alexandra Ohlsson, meteorologist on duty at Sweden’s SMHI weather forecaster, told Sweden's TT newswire.
In the 68 years since 1950, there has only been one year, 1986, when a tropical night has been recorded similarly early, in Kullen, also on Sweden’s West coast -- but that was two days later on June 4.
Last year, there was no tropical night at all, in 2016 it came on July 24, and in 2015 on July 2.
SMHI tweeted the news of the unusually early warmth.
from:
www.sunsail.com.au/blog/know-your-clouds
date 2018
June 5
time, 15:34
high level clouds
Cirrus clouds
So you’re sailing along under clear blue skies. You glance to port, and see no clouds; you swivel to starboard, nada. Then, you look over the bow once more, and in the far distance you see long, wispy streaks of cloud high in the sky. These, my friend, are Cirrus clouds, sometimes known as mare‘s tails.
Though they won’t leak on you, they indicate the arrival of a potentially wet warm front, so take note of their speed and direction. If they are heading to the east, you’re in luck, and fair weather is on its way. If not, you may be in for some rain and strong wind before things brighten up.
The stratosphere is very high up, it's the highest level and the main reason why high level winds are at their strongest ,meaning that the whole of the oxygen cycle from one side of the planet as in daylight to the other side of night relies on this wind power to make the Earth breathe. It inhales in the night and exhales in the day and then breathes in again and exhales again during the next day.
So at some 2 or 3 days after the tropical day, the stratosphere has displaced through the day into night about 3 times, meaning the amount of wind needed for the appearance of the tropical
Cirrus clouds = 3 days and nights of stratosphere wind motion.
The stratosphere clouds are also ,not usual in Scandinavia.
from Wikipedia
date 2018
June 5
time, 15:34
The stratosphere (/ˈstrætəˌsfɪər, -toʊ-/[3][4]) is the second major layer of Earth's atmosphere, just above the troposphere, and below the mesosphere. About 20% of the atmosphere's mass is contained in the stratosphere. The stratosphere is stratified in temperature, with warmer layers higher and cooler layers closer to the Earth. The increase of temperature with altitude is a result of the absorption of the Sun's ultraviolet radiation by the ozone layer. This is in contrast to the troposphere, near the Earth's surface, where temperature decreases with altitude. The border between the troposphere and stratosphere, the tropopause, marks where this temperature inversion begins. Near the equator, the stratosphere starts at 18 km (59,000 ft; 11 mi); at mid latitudes, it starts at 10–13 km (33,000–43,000 ft; 6.2–8.1 mi) and ends at 50 km (160,000 ft; 31 mi); at the poles, it starts at about 8 km (26,000 ft; 5.0 mi). Temperatures vary within the stratosphere with the seasons, in particular with the polar night (winter). The greatest variation of temperature takes place over the poles in the lower stratosphere; variations at lower latitudes and higher altitudes are smaller. Winds in the stratosphere can sometimes exceed 300 MPH, relative to the ground.
So at some 2 or 3 days after the tropical day, the stratosphere has displaced through the day into night about 3 times, meaning the amount of wind needed for the appearance of the tropical
Cirrus clouds = 3 days and nights of stratosphere wind motion.
The stratosphere clouds are also ,not usual in Scandinavia.
from Wikipedia
date 2018
June 5
time, 15:34
The stratosphere (/ˈstrætəˌsfɪər, -toʊ-/[3][4]) is the second major layer of Earth's atmosphere, just above the troposphere, and below the mesosphere. About 20% of the atmosphere's mass is contained in the stratosphere. The stratosphere is stratified in temperature, with warmer layers higher and cooler layers closer to the Earth. The increase of temperature with altitude is a result of the absorption of the Sun's ultraviolet radiation by the ozone layer. This is in contrast to the troposphere, near the Earth's surface, where temperature decreases with altitude. The border between the troposphere and stratosphere, the tropopause, marks where this temperature inversion begins. Near the equator, the stratosphere starts at 18 km (59,000 ft; 11 mi); at mid latitudes, it starts at 10–13 km (33,000–43,000 ft; 6.2–8.1 mi) and ends at 50 km (160,000 ft; 31 mi); at the poles, it starts at about 8 km (26,000 ft; 5.0 mi). Temperatures vary within the stratosphere with the seasons, in particular with the polar night (winter). The greatest variation of temperature takes place over the poles in the lower stratosphere; variations at lower latitudes and higher altitudes are smaller. Winds in the stratosphere can sometimes exceed 300 MPH, relative to the ground.
View from space of the stratosphere clouds.
Shown here is the layer of the WINDS as the STRATOSPHERE where heat regulation creates the change in atmospheric pressure the fastest way by the heat of the Sun so they are basically in the gas state of H2O but in motion dues to the change in day light to night time.
The interval is the input of NEEDED TROPICAL humidity that occurs in tropical climates, but is seldom seen in Scandinavia, perhaps every
70 years.
The types of chemicals that are active in the HUMIDITY are defined below.
from:http://acmg.seas.harvard.edu/people/faculty/djj/book/bookhwk11.html
date 2018
June 5
time, 15:34
Acetone in the upper troposphere
Recent measurements have revealed the ubiquitous presence of high concentrations of acetone in the upper troposphere, raising interest in the possible implications for tropospheric O3. Acetone is emitted to the atmosphere by both biogenic and anthropogenic sources, and is removed from the atmosphere mainly by photolysis (l < 360 nm). Consider the following mechanism for complete oxidation of acetone to CO2 in the atmosphere:
11. 6 Transport, rainout, and chemistry in the marine upper troposphere
We consider a simple dynamical model for the upper troposphere over the tropical oceans where direct transfer from the lower troposphere to the upper troposphere by deep convective clouds is balanced by large-scale subsidence. Let kij represent the first-order rate constant for transfer of air from layer i to layer j.
11. 7 Bromine chemistry in the troposphere
Events of rapid O3 depletion are observed in arctic surface air in spring, with concentrations dropping from 40 ppbv (normal) to less than 5 ppbv in just a few days. These O3 depletion events are associated with elevated bromine which appears to originate from the volatilization of sea salt bromide deposited on the ice pack. In this problem we examine the mechanism for Br-catalyzed O3 loss thought to operate in arctic surface air. Consider a surface air parcel in the arctic at the onset of an O3 depletion event. The air parcel contains 40 ppbv O 3 , 50 pptv Bry (sum of Br, BrO, HOBr, and HBr), 10 pptv CH 2 O, 3x107 molecules cm-3 HO2, and 1x10 5 molecules cm -3 OH. The air density in the parcel is 3x10 19 molecules cm -3 . Bromine chemistry is described by the reactions:
Shown here is the layer of the WINDS as the STRATOSPHERE where heat regulation creates the change in atmospheric pressure the fastest way by the heat of the Sun so they are basically in the gas state of H2O but in motion dues to the change in day light to night time.
The interval is the input of NEEDED TROPICAL humidity that occurs in tropical climates, but is seldom seen in Scandinavia, perhaps every
70 years.
The types of chemicals that are active in the HUMIDITY are defined below.
from:http://acmg.seas.harvard.edu/people/faculty/djj/book/bookhwk11.html
date 2018
June 5
time, 15:34
Acetone in the upper troposphere
Recent measurements have revealed the ubiquitous presence of high concentrations of acetone in the upper troposphere, raising interest in the possible implications for tropospheric O3. Acetone is emitted to the atmosphere by both biogenic and anthropogenic sources, and is removed from the atmosphere mainly by photolysis (l < 360 nm). Consider the following mechanism for complete oxidation of acetone to CO2 in the atmosphere:
11. 6 Transport, rainout, and chemistry in the marine upper troposphere
We consider a simple dynamical model for the upper troposphere over the tropical oceans where direct transfer from the lower troposphere to the upper troposphere by deep convective clouds is balanced by large-scale subsidence. Let kij represent the first-order rate constant for transfer of air from layer i to layer j.
11. 7 Bromine chemistry in the troposphere
Events of rapid O3 depletion are observed in arctic surface air in spring, with concentrations dropping from 40 ppbv (normal) to less than 5 ppbv in just a few days. These O3 depletion events are associated with elevated bromine which appears to originate from the volatilization of sea salt bromide deposited on the ice pack. In this problem we examine the mechanism for Br-catalyzed O3 loss thought to operate in arctic surface air. Consider a surface air parcel in the arctic at the onset of an O3 depletion event. The air parcel contains 40 ppbv O 3 , 50 pptv Bry (sum of Br, BrO, HOBr, and HBr), 10 pptv CH 2 O, 3x107 molecules cm-3 HO2, and 1x10 5 molecules cm -3 OH. The air density in the parcel is 3x10 19 molecules cm -3 . Bromine chemistry is described by the reactions:
Here you may observe the VITALLY IMPORTANT layer between the STRATOSPHERE and the TROPOSPHERE.
Actually it defines the thermal currents that are important to know about when space shuttles launch and have to
go through this layer prior to the HIGHEST atmosphere where the Earths layer changes into open space.
So it's important not to be caught in the stratosphere wind currents. Most launches of the space shuttle occur with
the right "weather forecasts" for this layer.
Actually it defines the thermal currents that are important to know about when space shuttles launch and have to
go through this layer prior to the HIGHEST atmosphere where the Earths layer changes into open space.
So it's important not to be caught in the stratosphere wind currents. Most launches of the space shuttle occur with
the right "weather forecasts" for this layer.
The NASA LOGO shows the orbital of the space zone with the openings in the stratosphere and the red signifies the heat of the stratosphere as it displaces through this
high wind layer by way of the troposphere as the LAUNCH WINDOW.
ntrs.nasa.gov/search.jsp?R=19920045595
date 2018
June 5
time, 15:55
NASA TECHNICAL REPORT SERVER.
Turbulence indicators for Space Shuttle launches
Author and Affiliation:Susko, Michael(NASA Marshall Space Flight Center, Huntsville, AL, United States)
Abstract:A report on the research and analysis for identifying turbulent regions from the surface to 16 km for Space Shuttle launches is presented. The research demonstrates that the results from the FPS-16 radar/jimsphere balloon system in measuring winds can indicate the presence of or conditions ripe for turbulence in the troposphere and lower stratosphere. It is shown that atmospheric data obtained during the Shuttle launches by the rawinsonde in conjunction with the jimsphere provide the necessary meteorological data to compute aerodynamic parameters to identify turbulence.
Publication Date:Jan 01, 1992
Document ID:19920045595
(Acquired Nov 22, 1995)
Accession Number:92A28219
Subject Category:METEOROLOGY AND CLIMATOLOGY
Report/Patent Number:AIAA PAPER 92-0718
Document Type:Preprint
Publisher Information:United States
Financial Sponsor:NASA; United States
Organization Source:NASA Marshall Space Flight Center; Huntsville, AL, United States
Description:11p; In English
Distribution Limits:Unclassified; Publicly available; Unlimited
Rights:Copyright
NASA Terms:ATMOSPHERIC TURBULENCE; BALLOON-BORNE INSTRUMENTS; SPACE SHUTTLE PAYLOADS; TROPOSPHERE; TURBULENCE METERS; WINDS ALOFT; RAWINSONDES; SPACECRAFT LAUNCHING; STRATOSPHERE; TROPOPAUSE; WIND VELOCITY MEASUREMENT
Imprint And Other Notes:AIAA, Aerospace Sciences Meeting and Exhibit, 30th, Reno, NV, Jan. 6-9, 1992. 11 p.
Availability Source:Other Sources
The black out stage is the STRATOSPHERE entry.
The facts of the high winds creates the higher ZERO GRAVITY INTERACTIONS of motions of spaceships at this time.
Because the action reaction occurs with gravity = the zero sum.
There are higher level "zero gravity" as well. Meaning that the easy 1 zero gravity stage has the "HARD" gravity layers=
3 zero gravity states.These probably also exist with STAR SYSTEM LIMITS and the alternations to other STAR SYSTEM EDGES
as the BLACK out may define the ZERO SUM of the SUN LIGHT ,by the winds=zero gravity 1 + the zero gravity 2 + Sun light as =zero gravity sum 3 star light.
This may be seen when the space shuttle is in REENTRY as it starts to create friction with the stratosphere and the burn angle indicates the the spaceshuttle
uses the wind direction in the stratosphere to displace the burn away from it.
The facts of the high winds creates the higher ZERO GRAVITY INTERACTIONS of motions of spaceships at this time.
Because the action reaction occurs with gravity = the zero sum.
There are higher level "zero gravity" as well. Meaning that the easy 1 zero gravity stage has the "HARD" gravity layers=
3 zero gravity states.These probably also exist with STAR SYSTEM LIMITS and the alternations to other STAR SYSTEM EDGES
as the BLACK out may define the ZERO SUM of the SUN LIGHT ,by the winds=zero gravity 1 + the zero gravity 2 + Sun light as =zero gravity sum 3 star light.
This may be seen when the space shuttle is in REENTRY as it starts to create friction with the stratosphere and the burn angle indicates the the spaceshuttle
uses the wind direction in the stratosphere to displace the burn away from it.