EMS Annual Meeting Abstracts
Vol. 21, EMS2024-312, 2024, updated on 05 Jul 2024
https://doi.org/10.5194/ems2024-312
EMS Annual Meeting 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Thursday, 05 Sep, 18:00–19:30 (CEST), Display time Thursday, 05 Sep, 13:30–Friday, 06 Sep, 16:00|

Drought Monitoring and Analysis in Mainland Portugal 

Vanda Pires1 and Tânia Cota2
Vanda Pires and Tânia Cota
  • 1Portuguese Sea and Atmosphere Institute, I.P., Clima and Climate Change division, Lisboa, Portugal (vanda.cabrinha@ipma.pt)
  • 2Portuguese Sea and Atmosphere Institute, I.P., Clima and Climate Change division, Lisboa, Portugal (tania.cota@ipma.pt)

Climate describes how the atmosphere behaves over a long period of time informing us on the “average of weather”, as well as the description of other aspects of weather patterns and meteorological parameters’ distribution, including anomalous, rare and extreme events. Some examples of extreme weather or climate events include heat waves, cold waves, floods, extreme precipitation, drought, tornadoes and tropical cyclones (WMO-CCL, 2018).

Drought is a natural weather phenomenon that occurs in all climates and can differ greatly from other extreme events. Unlike other extreme events, such as floods, which are weather events that are immediately detectable, droughts develop slowly, making it difficult to determine the onset and end.

Portugal is a country with recurrent phenomena’s of drought, which creates the strong need for impact reduction strategies as an integral part of drought preparedness plans.

To better understand the risk of droughts in mainland Portugal, was used indices that rely on precipitation deficits and allows us to characterize and monitor drought in Portugal, determining drought onset, duration and intensity. In this study was used the PDSI (palmer Drought Severity Index), SPI (Standardized Precipitation Index), SMI (Soil Moisture Index).

These indices were computed using daily and monthly data and based on the recommendations of CCL task team on the definition of extreme weather and climate events: Threshold (is determined based on historical values of the index); Temporal (Station-level information on starting date, ending date, and duration of the event); Spatial (calculates the area affected, by providing the distribution of stations where the threshold was surpassed and uses a geographical information system (GIS) to determine the area affected by the event, the magnitude, and severity).

In order to characterize the drought events was used the following properties:

  • Magnitude: measures the departure from the threshold and reflects unusualness or extremity of the event.
  • Duration: defined by the time at which the event begin and end.
  • Extent: defined as the geographical area affected by the extreme event.
  • Severity: severity should indicate the potential damages and impacts that can be associated to the event. It is a combination of magnitude and persistence of a drought.

It is also aimed the framing of this extreme event with climate changes based on trend analyses and simulation of scenarios with variables such as precipitation, temperature and evapotranspiration.

How to cite: Pires, V. and Cota, T.: Drought Monitoring and Analysis in Mainland Portugal , EMS Annual Meeting 2024, Barcelona, Spain, 1–6 Sep 2024, EMS2024-312, https://doi.org/10.5194/ems2024-312, 2024.