What is the Atlantic Ocean current that makes the English climate relatively mild?

The North Atlantic Drift is a warm ocean current that originates from the Gulf Stream. As this current moves across the Atlantic Ocean towards the western coasts of Europe, including the UK, it brings with it warmer temperatures that significantly influence the climate. The North Atlantic Drift helps to moderate the weather, leading to milder winters and cooler summers compared to other regions at similar latitudes. This is particularly evident in cities like London, where the climate remains more temperate due to the influence of this current.

The North Pacific Current and the California Current are primarily located in the Pacific Ocean and do not have a direct effect on the climate of England. The Equatorial Current operates near the equator and is associated with tropical weather patterns, which are also not relevant to the climate patterns in the UK. Thus, the North Atlantic Drift is clearly the current that plays a key role in creating a relatively mild English climate.