Revisiting the CMIP5 Thermocline in the Equatorial Pacific and Atlantic Oceans

Abstract The thermocline is defined as the ocean layer for which the vertical thermal gradient is maximum. In the equatorial ocean, observations led to the use of the 20 °C isotherm depth (z20) as an estimate of the thermocline. This study compares z20 against the physical thermocline in the equator...

Бүрэн тодорхойлолт

Номзүйн дэлгэрэнгүй

Үндсэн зохиолчид:	A. Castaño‐Tierno, E. Mohino, B. Rodríguez‐Fonseca, T. Losada
Формат:	Artigo
Хэл сонгох:	Inglês
Хэвлэсэн:	Wiley 2018-12-01
Цуврал:	Geophysical Research Letters
Нөхцлүүд:	thermocline model biases equatorial ocean Kuroshio intrusion northern South China Sea
Онлайн хандалт:	https://doi.org/10.1029/2018GL079847
Шошгууд:	Шошго нэмэх Шошго байхгүй, Энэхүү баримтыг шошголох эхний хүн болох!