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    El Niño Southern Oscillation (ENSO) region sea surface temperature forecasts

    Climate centres use several standard regional averages of sea surface temperature anomalies as indices to monitor the state of the equatorial Pacific ocean, especially anomalous warming/cooling associated with El Niño and La Niña

    to significant socio-economic impacts affecting infrastructure, agriculture, health and energy sectors for example. The name 'El Niño' nowadays is widely used specifically for the anomalous sustained warming of sea surface temperature that occurs every few years, typically concentrated in the central-east

  • prasanta_kumar_bal_2014_india.pdf

    to be driven by time-dependent large-scale fields (e.g. wind, temperature, water vapour, surface pressure, and sea-surface temperature (SST) at model sea grid-boxes) at their boundaries; this information is provided by a version of the Hadley Centre GCM, HadCM3 (Gordon et al. 2000; Collins et al. 2001

  • theor_appl_clim_tamil_nadu_india_precis.pdf

    , water vapour, surface pressure, and sea-surface temperature (SST) at model sea grid-boxes) at their boundaries; this information is provided by a version of the Hadley Centre GCM, HadCM3 (Gordon et al. 2000; Collins et al. 2001). HadCM3 was one of the major models used in the IPCC Third and Fourth

  • theor_appl_clim_tamil_nadu_india_precispdf

    , water vapour, surface pressure, and sea-surface temperature (SST) at model sea grid-boxes) at their boundaries; this information is provided by a version of the Hadley Centre GCM, HadCM3 (Gordon et al. 2000; Collins et al. 2001). HadCM3 was one of the major models used in the IPCC Third and Fourth

  • prasanta_kumar_bal_2014_indiapdf

    to be driven by time-dependent large-scale fields (e.g. wind, temperature, water vapour, surface pressure, and sea-surface temperature (SST) at model sea grid-boxes) at their boundaries; this information is provided by a version of the Hadley Centre GCM, HadCM3 (Gordon et al. 2000; Collins et al. 2001

  • Briefing on Arctic and Antarctic sea ice - June 2021

    -present, according to the NCEP reanalysis (Kalnay et al., 1996).   Figure 5. Near-surface meteorological conditions for November 2020 – March 2021 relative to the 1981-2010 long-term average: (a) mean sea level pressure anomaly (hPa); (b) surface air temperature anomaly (°C). Data are from the NCEP

  • Briefing on Arctic and Antarctic sea ice - June 2020

    and the Fram Strait). Figure 4. Surface meteorological conditions relative to the 1981-2010 average for November 2019 – March 2020: (a) mean sea level pressure anomaly (hPa); (b) surface air temperature anomaly (°C). Data are from the NCEP reanalysis (Kalnay et al, 1996). Although mild relative to the 1981

  • Kuniko_Yamazaki_ppt.pptx

    Precip - evap Winter mean sea level pressure Summer surface net downward SW Step 1&2 Result: 6 key drivers of AMOC strength were identified Extremely large river outflow E-P +ve region Step 3.1: Using proxy drivers from atmosphere-only PPE data that represent coupled surface fluxes, built

  • Met Office daily weather: High pressure building through the week

    High pressure is set to build across the UK this week, providing some calmer conditions

    . Temperatures are expected to be closer to the seasonal average than on Monday, but it will still feel pleasantly warm in any sunshine that does occur. High pressure will build across the UK this week, eventually providing many of us with calm conditions But calm doesn't automatically mean sunny

  • caa-case-study-4---high-pressure---winter-flight-gamet.pdf

    Scotland. Anticyclones normally bring settled weather, however the seasons and origin of the airmass often result in differences in cloud cover. For example, whilst we associate high pressure as bringing fine sunny weather to the UK during the summer, the same high pressure can lead to extensive

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