Alicante ends seven-day storm with just 0.5 liters of rain

A forum user reports Alicante received 0.5 liters per square meter during a week-long storm, while inland Valencia recorded 80 liters daily.

English · Original discussion in Spanish · Published

Alicante ends seven-day storm with just 0.5 liters of rain
Alicante ends seven-day storm with 0.5 liters of rain

Seven days of warnings. Seven days of maps showing green patches over the province. And finally, according to a forum user, the rain gauge for much of Alicante ended the episode with 0.5 liters per square meter. Half a liter. What fits in a small bottle, spread over an entire territory. Meanwhile, inland Valencia logged days of 50 and 80 liters, and storms in Marina Alta ranged between 300 and 500, while the rest of the province witnessed yet another cold drop that didn't arrive.

The sequence repeats with a punctuality that no longer surprises anyone. A week out, models predict 20 liters. Three days out, 15. One day out, 10. The same day, a bit of cloud. And finally, nothing. The result, in bad years, is a province closing the year with 160 liters annually, below much of Yemen. In good years, 250. The range is so wide that any average hides a simpler reality: it doesn't rain here, or it rains all at once and poorly.

Why orography doesn't explain Alicante's drought

The geographical argument falls apart. Alicante's orography is not so different from Valencia's, yet the water distribution is brutally unequal. The inland regions of Valencia accumulate episodes of 50, 80, and even 100 liters in 40 hours. Vega Baja experienced its last serious episode in September 2019. In the central and mountainous regions, the last decent rain—about 100 liters in 40 hours, not a huge amount—dates back to the spring of 2021.

The technical explanation points to the position of the cold air pocket. A DANA (Depression at High Levels, or isolated low pressure) does not guarantee water: it depends on where the core is placed, how it interacts with the Mediterranean, and whether the moist flow enters where it should. When it enters, it falls. When it doesn't, the sky stays gray, the alert sounds on your phone, and not a drop falls. The difference between a historic episode and an anecdote is decided in a few kilometers.

The red alert that sounded for nothing

The management of alerts also leaves a trail of skepticism. Some remember red alerts with normal storms the day before and absolute dryness the next. The phone rings, the alert activates, and the sky responds with a bird's pee. This mismatch between the alert and the result has a cost: when the real episode comes, half the population will have learned to ignore the alert.

This autumn episode also left an uncomfortable data point: 28 degrees at ten at night in October. A thermometer typical of the Persian Gulf in a province that, on paper, should have wet and stormy autumns. The combination of nighttime heat and lack of precipitation reinforces the feeling that the climate calendar has shifted.

The last strong cold drop was in 1997

The province's meteorological memory has two dates engraved. The last really strong cold drop occurred in 1997, with 270 liters per square meter. In 2025, the most relevant episode amounted to just 70 liters. Between the two, there are almost three decades of intermittent droughts, minor episodes, and storms that stayed at sea.

This shift toward the sea is another piece of the puzzle. Some argue that much of the water that should have fallen over the province was discharged directly into the Mediterranean. 600 liters per square meter fell into the sea in one of the recent episodes, according to records managed by weather enthusiasts. Water that irrigates nothing, fills no reservoirs, and cannot be counted as a resource.

Climate denialism and the theory of manipulation

At the opposite end of meteorological data is the theory of climate manipulation. A minority current maintains that the drought is not natural, but induced, and that someone—never clearly who—is diverting precipitation. These claims circulate without any evidence supporting them and rely on the coincidence that the Cantabrian coast also rains less than before. The scientific community does not endorse any of these hypotheses.

The contrast with other parts of Spain is inevitable. While the Northern Meseta, Galicia, and the Basque Country logged two consecutive weeks of rain, Alicante closed its latest episode dry. The comparison stings and fuels the sense of territorial grievance, but also hides a broader reality: the Spanish Mediterranean is entering a more extreme precipitation regime, with fewer rainy days and more concentrated episodes.

What happens when it finally rains

When water arrives, it doesn't arrive well. The province goes from absolute drought to flooding in hours. There is no middle ground. The episodes of 300 to 500 liters recorded in Marina Alta or Vega Baja demonstrate this: dry soil does not absorb, water runs off, and the result is a catastrophe. Drought and flooding are the two sides of the same problem.

The underlying debate is whether this province has a climatic future. With 160 liters annually in bad years, any agricultural or industrial activity depending on water enters a zone of risk. Desalination covers part of the deficit, but at an energy cost that cannot compete with rain. And meanwhile, the calendar keeps advancing: another autumn without a serious episode, another winter without a winter, another spring waiting for a storm that never comes.

The analysis gets stuck exactly here. The data says water falls farther away, more concentrated, and later. Orography is not enough to explain it. Alert management does not help. And the unanswered question is the most uncomfortable of all: if this is the new normal, how long can an entire province endure waiting for a drop that never falls?

Summary of a discussion on Burbuja.info - Foro de economía, actualidad y política., translated from Spanish and reviewed before publication. Read the full discussion (58 replies).

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