Time to reach glucose <14 mM was 7 (1 to 15) hours with a fall rate of 3.7 (2.9 to 6.8) mM/hour.
An infiltration rate of 15 mm/hour means that a water layer of 15 mm on the soil surface, will take one hour to infiltrate.
During this period 94 mm of rainfall was recorded (1.3-year return period), half fell within a 2-hour period at an intensity of 25 mm/hour while the maximum hourly rainfall intensity reached 37 mm/hour (return period 1.8 years)t (from Table 1).
The 64-m dish provides a gain of 72.5 dBi including the feeder loss in X-band, at a system noise temperature of 96 K for a 5 mm hour−1 rain and an elevation angle of 15°.
Column 7 indicates the infiltration rate (in mm/hour); this is the infiltration rate (in mm/minute, column 6) multiplied by 60 (60 minutes in 1 hour).
Potassium during treatment was 4 (3.2 to 5.2) mM and required 35 (12 to 60) mM/hour to maintain the target 3.5 to 5 mM.
The "normal" upper limit of 20 mm/hour for Westergren sedimentation rate was also the optimal limit of normal by receiver operating characteristic analysis of the study population.
This suggests that rolling hill country in pastoral use (~5% of the study area) was peripheral to the storm centre with rainfall intensities below the 25 mm/hour threshold required to trigger shallow landslides (Caine 1980).
Laboratory tests showed haemoglobin of 5.6 mmol/L, raised ESR of 110 mm/hour, CRP of 74 mg/L (reference range, 0 to 8 mg/L), normal liver function tests, and QuantiFeron negative.
The median values were 20 mm/hour in cases and 9 mm/hour in controls.
