Pollen allergy in the Bilbao area (European Atlantic seaboard climate): pollination forecasting methods
- 1 February 1995
- journal article
- Published by Wiley in Clinical and Experimental Allergy
- Vol. 25 (2) , 133-140
- https://doi.org/10.1111/j.1365-2222.1995.tb01018.x
Abstract
Summary: Forecasting pollination can help the allergist to establish the appropriate treatment and advice for patients. Based on previous studies, we have related the climate variables with the grass pollen counts in the search for pollination predictors. By relating the meteorological data of the temperature recorded every 6h and of the rainfall in hourly periods, together with the daily pollen counts obtained by the Hirst volumetric system, over a period of 3 years, we have tried to predict the start, duration and severity of the grass pollination, as well as the days of peak pollination. We have established a relationship by means of a polynomic regression originating from the mean cumulated temperature higher than 9°C [R2= 0.927 (P= 0.0001)], with the pollination season starting from 300°C and the maximum peak at 356°C, in the 3 years of the study. During the days of pollination, peaks higher than 50 grains/m3 coincide with average daily temperatures of 18.7±3 and lower than 50 grains/m3 with temperatures of 16.8 ± 3 (significant to 95%). The duration of the pollination is influenced by the cumulated average temperatures (from 800 to 900°C) and especially by precipitation at the start of and during pollination. In order to forecast grass pollination, the cumulated average temperatures are useful, starting from a basal (9°C), pollination begins when this sum is greater than 300°C, whereas when 800°C is reached and depending on the rainfall during the season, pollination will end. The total severity of pollination seems to depend on the rainfall prior (in the same year) to the start. During pollination, the days with an average temperature of 18.7 ± 3°C and an absence of rainfall between 4 and 12 h, will be the days with a presence of more than 50 grains/m3. Thus, it is possible to forecast and estimate risk factors in the long‐term (by means of the rainfall prior to pollination) and in the short‐term (for the following day, if a weather forecast is available) so as to offer it to those members of the population affected by pollinosis.Keywords
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