The Intertropical Convergence Zone (ITCZ) is a global-scale band of tropical precipitation lying, in the annual mean, just north of the equator. Its position can be tied to the atmosphere's energy balance: the Northern Hemisphere is heated more strongly than the Southern Hemisphere, biasing the atmosphere's circulation and ITCZ north of the equator. In the context of this energy balance framework, we examine multidecadal connections between variations in the position of the global ITCZ and indices of extratropical sea surface temperature (SST) variability over the twentieth century. We find that the ITCZ and atmospheric circulation are shifted farther to the north during periods when North Atlantic and North Pacific SSTs are anomalously war...
Across a range of simulations with a coupled atmosphere–ocean climate model, shifts in the intertrop...
The interannual variability of the location of the intertropical convergence zone (ITCZ) is strongly...
Millennial-scale climate oscillations of the last glacial, called Dansgaard/Oeschger (D/O) cycles, h...
Rainfall on Earth is most intense in the intertropical convergence zone (ITCZ), a narrow belt of clo...
We examine the link between migrations in the intertropical convergence zone (ITCZ) and changes in t...
Rainfall on Earth is most intense in the intertropical convergence zone (ITCZ), a narrow belt of clo...
Tropical hydroclimate is modulated by the position and intensity of the Intertropical Convergence Zo...
The authors quantify the relationship between the location of the intertropical convergence zone (IT...
Shifts in the position of the intertropical convergence zone (ITCZ) have great importance for weathe...
The Intertropical Convergence Zone (ITCZ) is a feature that results from the ocean-atmosphere intera...
The intertropical convergence zone (ITCZ) in the east Pacific is located north of the equator during...
The intertropical convergence zone (ITCZ) accounts for more than 30% of the global precipitation and...
The interannual variability of the location of the intertropical convergence zone (ITCZ) is strongly...
Tropical paleoclimate records provide important insights into the response of precipitation patterns...
The intertropical convergence zone (ITCZ) can shift meridionally on seasonal and longer time scales....
Across a range of simulations with a coupled atmosphere–ocean climate model, shifts in the intertrop...
The interannual variability of the location of the intertropical convergence zone (ITCZ) is strongly...
Millennial-scale climate oscillations of the last glacial, called Dansgaard/Oeschger (D/O) cycles, h...
Rainfall on Earth is most intense in the intertropical convergence zone (ITCZ), a narrow belt of clo...
We examine the link between migrations in the intertropical convergence zone (ITCZ) and changes in t...
Rainfall on Earth is most intense in the intertropical convergence zone (ITCZ), a narrow belt of clo...
Tropical hydroclimate is modulated by the position and intensity of the Intertropical Convergence Zo...
The authors quantify the relationship between the location of the intertropical convergence zone (IT...
Shifts in the position of the intertropical convergence zone (ITCZ) have great importance for weathe...
The Intertropical Convergence Zone (ITCZ) is a feature that results from the ocean-atmosphere intera...
The intertropical convergence zone (ITCZ) in the east Pacific is located north of the equator during...
The intertropical convergence zone (ITCZ) accounts for more than 30% of the global precipitation and...
The interannual variability of the location of the intertropical convergence zone (ITCZ) is strongly...
Tropical paleoclimate records provide important insights into the response of precipitation patterns...
The intertropical convergence zone (ITCZ) can shift meridionally on seasonal and longer time scales....
Across a range of simulations with a coupled atmosphere–ocean climate model, shifts in the intertrop...
The interannual variability of the location of the intertropical convergence zone (ITCZ) is strongly...
Millennial-scale climate oscillations of the last glacial, called Dansgaard/Oeschger (D/O) cycles, h...