Solar Insolation - Explaining Why It's Hotter North Of Tropics In Summer & How It Can Get Hot By Arctic Circle. This is the 2nd part of the previous episode.

Become a supporter of this podcast: https://www.spreaker.com/podcast/weather-with-enthusiasm--4911017/support.

This episode discusses heat in Russia including Siberia, Astrakhan and the Caspian Sea.

Become a supporter of this podcast: https://www.spreaker.com/podcast/weather-with-enthusiasm--4911017/support.

This Episode Discusses How Extreme Heat Takes Place In The Arctic And The Higher Latitudes

Become a supporter of this podcast: https://www.spreaker.com/podcast/weather-with-enthusiasm--4911017/support.

Ever wondered why some regions are hotter than others, and how heatwaves can reach as far north as Siberia? In this fascinating episode, we uncover the science behind summer temperatures and reveal how the tilt of the Earth is connected to the recent heatwave in Siberia. Join us as we explore the differences between tropical and subtropical climates, and venture into the scorching Death Valley, California, an ideal geographical location for soaring temperatures. We also take a deep dive into the complex dynamics of the sun's ability to heat temperatures in the northern latitudes. With the help of the solar insolation chart from the National Weather Service, we investigate how the length of the day and the sun's angle in the sky can affect temperatures at the Arctic Circle and North Pole—even when there's no nighttime! Discover why temperatures in the Arctic can be hotter than in the southern parts of the world, and how an air mass at 44 degrees north latitude can impact other latitudes. Lastly, we delve into the historical heatwaves and the role of greenhouse gases in causing extreme heat in the northern latitudes. Learn about the Earth's response to the sun's increasing heat and how it can affect temperatures over a three-to-four-week period. We also discuss the disproportionate warming of the Arctic and its impact on the jet stream, and the vital importance of contrast in temperatures. Don't miss this enlightening and informative episode that will change the way you think about summer temperatures and heatwaves

Become a supporter of this podcast: https://www.spreaker.com/podcast/weather-with-enthusiasm--4911017/support.

We've got some mind-blowing weather news to share with you! The El Nino has arrived and it's even stronger than predicted, with potential impacts on our climate for the upcoming year. On this thrilling episode of Weather with Enthusiasm, we'll also discuss other weather headlines like scorching heat, air quality challenges from wildfires and volcanic eruptions, and the shocking Siberian heat wave. Plus, we'll touch on the unusual excessive heat warnings in San Juan, Puerto Rico - something that's rarely seen!
Don't miss out on this fascinating episode of Weather with Enthusiasm, where we'll delve into the hottest topics literally!

Become a supporter of this podcast: https://www.spreaker.com/podcast/weather-with-enthusiasm--4911017/support.

Headlines: A Historic Siberian Heatwave Shocker...., EL Nino becomes official....Excessive and record breaking heat in Puerto Rico continues with 125° Heat index....Volcano erupts in low altitude causing intense air pollution....the eruption is ongoing.

Become a supporter of this podcast: https://www.spreaker.com/podcast/weather-with-enthusiasm--4911017/support.

The summertime Ridge (dome of heat) developed further north than usual this year. This is likely due to a series of low pressure systems that were in the south. The low pressure in the south also prevented the warm moist flow on the back side of the Bermuda high from influencing the United States and limited thunderstorm activity to the north. Therefore, the dome of heat had less moisture to work with. Dew points approached 60° in many places and even 70° in Minnesota last week. Although this is somewhat humid it falls well short of the norm especially for the more southern cities. Rapid onset drought developed in many locations especially over the Midwest cornbelt from Iowa eastward into the Ohio Valley and northward. Being that this is the 3rd stagnant airmass of warm and dry air that expanded into Canada this year, conditions were drier than usual. The September hurricane downed trees in Nova Scotia. These dry dead trees provide ample fuel for fire in Nova Scotia.  The combination of all this produced good fire weather. 

(The other 2 ingredients which allow for rapid fire spread are dry thunderstorms and wind. )


It is not clear why the wild fires are 7 times worse than usual in Canada this year. Regardless as to what the cause of such intensity is, a stationary low pressure system over the gulf of Maine brought a steady flow of winds from southern Canada into the United States. This brought horrific levels of smoke down to the surface across many of the major cities in the Mid-Atlantic area and the northeast. Fortunately for the northeast stagnant northeast winds are not common in the Summer season. 


Although the intensity of the smoke in New York became well known, the smoke in Bismarck, North Dakota last month was 3x worse in many ways as the visibility dropped to a blinding 0.25 miles at times. In Chicago the smoke blocked out the Sun to a mere moon like figure which was colored pink around May 18th. Fortunately for Chicago much of the smoke remained above the surface. 

In this episode we reiterate the unique synoptic setup that occured in the Midwest and southern Canada last week as summer heat blew in with

northeast winds. 

Although it is not clear at this time whether the northeast component to this wind from this airmass effected the fire spread in Canada in an unusual way, it is clear that stagnant domes of heat help the spread of wild fires. 


It is key to point out that shortly before northeast winds blew hot dry air into the Midwest, there was a stationary high pressure system over New England. (At that time it was producing southeasterly winds in much of the the Midwest. ) This stagnant air likely played a roll in the spread of wildfire in Nova Scotia. 
While it is well established that there is a connection between domes of heat and wild fire spread, in this episode we try to make an additional connection between last week's dome of heat in particular. This was done in an attempt to explain the unprecedented intensity of the wildfires currently in Canada. However, the information presented in this episode is not set in stone as of yet. 

Become a supporter of this podcast: https://www.spreaker.com/podcast/weather-with-enthusiasm--4911017/support.

Ever wondered what's causing the recent surge in the unusually thick smoke across parts of the United States such as in New York? Join us as we attempt to unravel this mystery.
In this episode, we explore the connection between two stagnant air masses in the region and how this weather pattern is rare for the Summer. This synoptic setup could be contributing to the intensity of the influx of wildfire smoke from Canada into areas like New York, Pennsylvania, and even major cities like Baltimore and Washington DC.

We also delve into the complexities of our ever-changing weather and it's domino effect. Discover how rain was removed from the forecast due to the stability that smoke provides in the upper atmosphere.
Don't miss this fascinating episode!

Become a supporter of this podcast: https://www.spreaker.com/podcast/weather-with-enthusiasm--4911017/support.

Become a supporter of this podcast: https://www.spreaker.com/podcast/weather-with-enthusiasm--4911017/support.

Become a supporter of this podcast: https://www.spreaker.com/podcast/weather-with-enthusiasm--4911017/support.