Results 11 to 20 of about 802 (155)
Diagnosing Ocean Feedbacks to the BSISO: SST‐Modulated Surface Fluxes and the Moist Static Energy Budget [PDF]
AbstractThe oceanic feedback to the atmospheric boreal summer intraseasonal oscillation (BSISO) is examined by diagnosing the sea surface temperature (SST) modification of surface fluxes and moist static energy on intraseasonal scales. SST variability affects intraseasonal surface latent heat (LH) and sensible heat (SH) fluxes, through its influence on
Yingxia Gao +3 more
semanticscholar +7 more sources
The Boreal Summer Intraseasonal Oscillation (BSISO) is a prominent tropical intraseasonal variability during summer. It propagates northeastward from the northern Indian Ocean to the western North Pacific and has a more complex structure than the winter ...
Yuki Maeda, Masaki Satoh
doaj +3 more sources
Northward Propagating Versus Non‐Propagating BSISO Over South Asia: Horizontal Advection Driven Moisture Mode Within a Vertically Sheared Background [PDF]
AbstractThe Boreal Summer Intraseasonal Oscillation (BSISO) is a pronounced mode of tropical variability. Here, we identify two types of BSISO events, one which propagates northward over South Asia from the equatorial Indian Ocean (EIO), and the other which doesn't.
Sambrita Ghatak, Jai Sukhatme
semanticscholar +4 more sources
Impact of the observed SST frequency in the model initialization on the BSISO prediction [PDF]
AbstractThe impact of the observed sea surface temperature (SST) frequency in the model initialization on the prediction of the boreal summer intraseasonal oscillation (BSISO) over the Western North Pacific (WNP) is investigated using the Beijing Climate Center Climate System Model. Three sets of hindcast experiments initialized by the observed monthly,
Xueyan Zhu +5 more
openaire +2 more sources
Topographic Effects on the Luzon Diurnal Cycle during the BSISO [PDF]
AbstractCloud-resolving simulations are used to evaluate the importance of topography to the diurnal cycle (DC) of precipitation (DCP) over Luzon, Philippines, and surrounding ocean during the July–August 2016 boreal summer intraseasonal oscillation (BSISO) event.
Emily M. Riley Dellaripa +4 more
openaire +2 more sources
Propagation Characteristics of BSISO Indices [PDF]
AbstractThe spatial structure and propagation of tropical intraseasonal convection anomalies diagnosed with the outgoing longwave radiation‐based Madden‐Julian Oscillation index are examined in the boreal summer and winter seasons. It is shown that the outgoing longwave radiation‐based Madden‐Julian Oscillation index represents both northward and ...
Shuguang Wang +3 more
openaire +2 more sources
The Indian summer monsoon in MetUM-GOML2.0: effects of air–sea coupling and resolution [PDF]
The fidelity of the simulated Indian summer monsoon is analysed in the UK Met Office Unified Model Global Ocean Mixed Layer configuration (MetUM-GOML2.0) in terms of its boreal summer mean state and propagation of the boreal summer intraseasonal ...
S. C. Peatman, N. P. Klingaman
doaj +5 more sources
Propagating Mechanisms of the 2016 Summer BSISO Event: Air‐Sea Coupling, Vorticity, and Moisture
AbstractDuring the summer of 2016, a boreal summer intraseasonal oscillation (BSISO) event was observed over Southeast Asia and the South China and Philippine seas. Precipitation anomalies associated with this event propagated northward at a speed of 0.5–1° per day from July to August.
Shuguang Wang +6 more
openaire +3 more sources
The boreal summer intraseasonal oscillation (BSISO) is a major mode of sub‐seasonal variability that regulates the summer climate in East Asia. This study investigates the four possible effects of two different time‐scale BSISOs on temperature and ...
Yoo‐Rim Jung, Woo‐Seop Lee
doaj +2 more sources
The Boreal Summer Intraseasonal Oscillation (BSISO): A Review
The boreal summer intraseasonal oscillation (BSISO) is among the most pronounced subseasonal variability in the tropics during boreal summer. Compared with its wintertime counterpart, the so-called Madden–Julian oscillation (MJO), the BSISO convection ...
K. Kikuchi
openaire +3 more sources

