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presentations. The group(s) receiving the most votes can then present to their year group in an assembly or to members of the SLT. Bring the lesson to a close by coming together as a class to discuss how we can reduce the impacts of climate change – both on ourselves and other people around the world
and NHS inform. Dr Siama Latif, NHS 24’s Associate Medical Director said: “When the weather gets colder this can have an impact on everyone’s health and wellbeing, but especially those who could be considered vulnerable, such as the very young, the elderly, or those with long-term health conditions
to El Niño and La Niña relate only to sea-surface-temperature anomalies in the tropical Pacific Niño3.4 region (120°–170°W, 5°N–5°S). Our references to El Niño, neutral and La Niña conditions generally correspond to sea-surface-temperature (SST) anomalies >0.5°C, between -0.5 and +0.5°C, and <-0.5
(160°E-150°W, 5°S – 5°N), the forecast vs. observed temperature correlation is r=0.84 with a 0.67°C mean RMS error. Forecasts of sea surface temperature in the Atlantic are also skilful: in the tropical Atlantic formation region (5°-85°W, 10°N– 30°N), the forecast vs. observed temperature correlation
/s 0.00 0.03 0.09 0.28 0.90 Figure 4: A priori CH 4 emissions for 2007 interpolated onto the InTEM inversion grid. 5.4 Bayesian cost function and uncertainty elements The cost function within an inversion framework is the tool used to assess the best-fit of the a posteriori emissions and allows
in knots. The knot is defined as a speed of one nautical mile per hour. 1 knot = 0.51444 m s -1 = 1.15078 mile h -1 = 1.853 km h -1 = 1.689 ft s -1 There is a close relationship between surface isobars (line joining points of equal pressure) and wind speed and direction over open level terrain
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