Author: Isaac Gendler

Cloud Bases

Cloud Bases

Cloud Bases

06/06/25

“How do we describe the base of a cloud?”

Clouds come in all shapes and sizes. But how do we describe their lowest visible parts? Well, just like the beginning of any structure is called a “base”, the lowest visible region of a cloud is termed a Cloud Base. Cloud bases are measured as the distance from mean sea level or the Earth’s surface.

Nimbostratus Clouds

Nimbostratus Clouds

Nimbostratus Clouds

06/03/25

“How do we classify dark and moderately rainy clouds?”

Clouds come in all shapes and sizes. During warm fronts, moisture may rise into the atmosphere and create dark clouds. These Nimbostratus Clouds produce constant streams of rain with (usually) no lightning or thunder. Nimbostratus clouds typically form around 2 – 4 kilometers in the middle level of the troposphere.

Image credit: https://www.metoffice.gov.uk/

Garbage Patches in Ocean Gyres

Garbage Patches in Ocean Gyres

Garbage Patches in Ocean Gyres

06/02/25

“Why do country-sized garbage patches circle the oceans?”

Ocean gyres rotate water between continents like a conveyor belt. When people release garbage into the ocean, it can get sucked into this rotation. Over time, this waste has accumulated into giant Garbage Patches in Ocean Gyres. The largest by area, the Great Pacific Garbage Patch, is estimated to be around twice as large as the U.S. state of Texas! These garbage patches are not continuous, solid masses, but rather similar to a mirky soup soup.

Image credit: cdn.prod.website-files.com

Westerlies Seasonal Variation

Westerlies Seasonal Variation

Westerlies Seasonal Variation

06/01/25

“How do the westerlies have seasonal variation?”

The westerlies are a vital part of global air circulation. Temperature differences between the poles and tropics are one of the causes of these winds. During the winter, the temperature differences between these two regions are greater, leading to stronger westerlies winds. This is why Westerlies Seasonal Variation occurs. Storms in the westerlies regions are stronger during the wintertime as a consequence.

Cold Ocean Currents

Cold Ocean Currents

Cold Ocean Currents

05/29/25

“Why do some ocean currents carry cold water?”

Ocean currents carry water from all over the world. The sun’s position near the poles tends to bring cold water in these currents. These Cold Ocean Currents play a decisive role in the climate of nearby landmasses. If a cold ocean current is close to a landmass, it will cool the land and add moisture to the atmosphere. Because of global water circulation, cold ocean currents are more likely to form on the western side of continents than on the eastern side. Examples of Cold Ocean Currents include the California Current and the Benguela Current.