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met-office-data-products-and-services-brochure-july-2025pdf
levels (surface, atmosphere, specific level) - Pressure levels - Height levels - Depth levels API GRIB2 Met Office Weather DataHub Global Media delivery services A range of our data can be delivered through the media delivery services. For example, reviews of the UK weather, forecast guidance
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met-office-data-products-and-services-brochure-july-2025.pdf
levels (surface, atmosphere, specific level) - Pressure levels - Height levels - Depth levels API GRIB2 Met Office Weather DataHub Global Media delivery services A range of our data can be delivered through the media delivery services. For example, reviews of the UK weather, forecast guidance
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Place
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
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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
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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
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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
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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
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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
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High pressure brings plenty of sunshine and temperatures of 22°C
With high pressure becoming established this week, the start of April will be warm and sunny across the UK. With the area of high pressure situated to the northeast of the UK, there will be a strong breeze across the southern half of the UK through the start of the week. In windward coastal areas
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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