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Heatwave magnitude is estimated by means of the Heat Wave Magnitude Index daily14,31 (HWMId).
The effect of relative humidity on the heat wave magnitude and peak might even be underestimated here.
Climate model projections suggest that the percentage of area where heat wave magnitude and peak are amplified by humidity increases with increasing warming levels.
A heatwave is defined using the Heat Wave Magnitude Index daily14 (HWMId), which takes into account both duration and temperature anomalies of a heatwave into a single number.
A AHWI score twice as large as the one of the HWMId means that the heat wave magnitude is amplified twice by humidity.
Given the prevalence of mucosal wave magnitude and symmetry variations in the normophonic population, overdiagnosis may be possible without caution.
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Additionally, by using daily maximum temperature and minimum relative humidity outputs from the Coupled Model intercomparison Project Phase 5 (CMIP518), we project heat wave and apparent heat wave magnitudes at different warming levels (1.5°, 2° and 4°) relative to the period 1861 1880 (see method).
They had body wave magnitudes ranging from 4.3 to 4.5, local magnitudes between 3.7 and 4.2, and surface wave magnitudes of 3.7 to 3.9 (Ajakaiye et al. [1987]; Akpan and Yakubu [2010]; Eze et al. [2011]).
This assumes a direct link between rupture velocity along the fault and wave magnitudes at the seismometer.
Some of the surface wave magnitudes were lost/gained due to event depth recomputed to be deeper/shallower than 60 km (IASPEI 2005).
The most dramatic example of this is provided by "tsunami earthquakes", which are large tsunamigenic thrust faulting earthquakes that rupture shallow (<15 km) depths of megathrusts and have anomalously low surface wave and body wave magnitudes relative to their long-period moment magnitudes (Mw) (Kanamori, 1972).
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