Image 1 of 1

SPL TEMPERATURE INVERSION IN THE PEAK DISTRICT 05.jpg

Add to Cart Add to Lightbox Download
A couple watch a weather inversion form over the Hope Valley, from the summit of Mam Tor in the Peak District at sunrise on 21 September 2020. Normally air is warmest near the ground as the sun warms the land that heats up the air, and as elevation increases, the temperature drops. If this temperature gradient is reversed, with cold air nearest to the ground, the colder temperature causes moisture in the air to condense to form fog and mist. Picture by Matt Wilkinson/Stella Pictures Ltd 07814 960751
21/09/2020
Copyright
©Stella Pictures Limited https://www.stellapictures.co.uk +44 7813 022858
Image Size
2500x1664 / 959.3KB
https://www.stellapictures.co.uk
Contained in galleries
Temperature Inversion in the Peak District, Portfolio - News
A couple watch a weather inversion form over the Hope Valley, from the summit of Mam Tor in the Peak District at sunrise on 21 September 2020. Normally air is warmest near the ground as the sun warms the land that heats up the air, and as elevation increases, the temperature drops. If this temperature gradient is reversed, with cold air nearest to the ground, the colder temperature causes moisture in the air to condense to form fog and mist. Picture by Matt Wilkinson/Stella Pictures Ltd 07814 960751<br /> 21/09/2020