The depth of the thermocline in the west is somewhat limited
because oceanic warming can not continue indefinitely.
Not exact matches
«Our study is important
because tropical cyclone intensity forecasts for several past hurricanes over the Caribbean Sea have under - predicted rapid intensification events over
warm oceanic features,» said Johna Rudzin, a PhD student at the UM Rosenstiel School and lead author of the study.
It can not be seen directly
because of
oceanic damping, but it does call for about ~ 0.3 C of
warming (instead of ~ 0.1 C from pure TSI) in the early 20th century based on Lockwood's solar activity reconstructions.
Ponta Delgada has a borderline humid subtropical (Cfa) and Mediterranean climate (Csa) under the Köppen classification with strong
oceanic (Cfb) influence, due to high levels of precipitation throughout the year combined with less sunshine, and
because only one
warm month just reaches 22.1 °C (71.8 °F).
Original post Last summer, a paper published in Nature, «Global phytoplankton decline over the past century,» caught the attention of climate campaigners and some media outlets
because it concluded that
warming of the seas over the last century was linked with a big and near - global decline in
oceanic phytoplankton.
The difficulty arises
because oceanic sea - surface temperatures
warm up at a much slower rate than those above land.
Those temperatures are high simply
because they sit on top of that step
warming of
oceanic origin.
Because of the accumulation of greenhouse gases in the atmosphere, the
oceanic «conveyor belt» that sends
warmer waters into the North Atlantic could abruptly shut down.
Accelerated
oceanic conveyor belt can't be hidden
because the
warm side travels the surface out of the tropics and can be sounded cheaply.