Eastern Pacific Warm Pool paleosalinity and climate variability: 0-30 kyr
نویسندگان
چکیده
منابع مشابه
Climate and hydrographic variability in the Indo-Pacific Warm Pool during the last millennium
[1] Planktonic foraminiferal Mg/Ca and dO derived sea surface temperature and salinity records from the Makassar Strait, Indonesia, show a long-term cooling and freshening trend, as well as considerable centennial-scale variability during the last millennium. The warmest temperatures and highest salinities occurred during the Medieval Warm Period (MWP), while the coolest temperatures and lowest...
متن کاملHuman-caused Indo-Pacific warm pool expansion
The Indo-Pacific warm pool (IPWP) has warmed and grown substantially during the past century. The IPWP is Earth's largest region of warm sea surface temperatures (SSTs), has the highest rainfall, and is fundamental to global atmospheric circulation and hydrological cycle. The region has also experienced the world's highest rates of sea-level rise in recent decades, indicating large increases in...
متن کاملConvection and Easterly Wave Structures Observed in the Eastern Pacific Warm Pool during EPIC-2001
During September–October 2001, the East Pacific Investigation of Climate Processes in the Coupled Ocean– Atmosphere System (EPIC-2001) intertropical convergence zone (ITCZ) field campaign focused on studies of deep convection in the warm-pool region of the eastern Pacific. This study combines C-band Doppler radar, sounding, and surface heat flux data collected aboard the R/V Ronald H. Brown dur...
متن کاملWestern Pacific Warm Pool and ENSO Asymmetry in CMIP3 Models
Theoretical and empirical studies have suggested that an underestimate of the ENSO asymmetry may be accompanied by a climatologically smaller and warmer western Pacific warm pool. In light of this suggestion, simulations of the tropical Pacific climate by 19 Coupled Model Intercomparison Project Phase 3 (CMIP3) climate models that do not use flux adjustment were evaluated. Our evaluation reveal...
متن کاملVariability of sea surface temperature and warm pool area in the South China Sea and its relationship to the western Pacific warm pool
Sea surface temperature (SST) data derived from satellite and in situ measurements are used to study the thermal variability in the South China Sea (SCS). Time–frequency–energy distributions, periods of variability, and trends are computed by the Hilbert–Huang transform method. The SST trend from 1982 to 2005 is 0.276 C per decade in the SCS which is higher than 0.144 C per decade in the wester...
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ژورنال
عنوان ژورنال: Paleoceanography
سال: 2006
ISSN: 0883-8305
DOI: 10.1029/2005pa001208