Dynamic Ocean-Atmosphere Coupling: A Thermostat for the Tropics
about
Twentieth-Century Sea Surface Temperature TrendsDynamical and cloud-radiation feedbacks in El Niño and greenhouse warmingCroll revisited: Why is the northern hemisphere warmer than the southern hemisphere?A westward extension of the warm pool leads to a westward extension of the Walker circulation, drying eastern Africa
P2860
Dynamic Ocean-Atmosphere Coupling: A Thermostat for the Tropics
description
1996 nî lūn-bûn
@nan
1996年の論文
@ja
1996年学术文章
@wuu
1996年学术文章
@zh-cn
1996年学术文章
@zh-hans
1996年学术文章
@zh-my
1996年学术文章
@zh-sg
1996年學術文章
@yue
1996年學術文章
@zh
1996年學術文章
@zh-hant
name
Dynamic Ocean-Atmosphere Coupling: A Thermostat for the Tropics
@en
Dynamic Ocean-Atmosphere Coupling: A Thermostat for the Tropics
@nl
type
label
Dynamic Ocean-Atmosphere Coupling: A Thermostat for the Tropics
@en
Dynamic Ocean-Atmosphere Coupling: A Thermostat for the Tropics
@nl
prefLabel
Dynamic Ocean-Atmosphere Coupling: A Thermostat for the Tropics
@en
Dynamic Ocean-Atmosphere Coupling: A Thermostat for the Tropics
@nl
P1433
P1476
Dynamic Ocean-Atmosphere Coupling: A Thermostat for the Tropics
@en
P304
P356
10.1126/SCIENCE.272.5265.1148
P407
P577
1996-05-01T00:00:00Z