2025.08.23 – METEOROLOGICAL EXTREMES AND INSTITUTIONAL ALERT STRUCTURES IN BAHÍA BLANCA, MARCH 2025

The analysis examines the structure of extreme rainfall, convective dynamics, and institutional warning systems during early March 2025 in Bahía Blanca.


EMPIRICAL ANALYSIS

● The National Meteorological Service (SMN) identifies a sequence of rainfall extremes between March 4 and March 8, 2025, with the peak on March 7 in Bahía Blanca.

● The atmospheric setting combines a surface low over Cuyo and the Northwest with a surface high in the South Atlantic.

● A high-level low advances from the Pacific and supports vertical motion, moisture accumulation, and thermal instability. 🌎

● A cold front enters from the northern Patagonia sector and triggers severe convection.

● Columns present precipitable water between 40 and 60 mm with convective available potential energy above 4000 J/kg.

● These parameters align with severe storms and intense rainfall. ⛈️

DYNAMICS AND TIMING

● Between 03:00 and 09:00 local time on March 7, convective cells concentrate over Bahía Blanca.

● GOES-16 infrared observations indicate organization and persistence of the convective system.

● Rainfall persists through the morning and decreases in the afternoon. 📉

● Recorded accumulation in Bahía Blanca reaches 312 mm between March 4 and March 8.

● A maximum of 290 mm falls in only 12 hours on March 7, equal to about 25 mm/h.

● The daily total of 210 mm between March 6 and March 7 surpasses the previous record of 150.9 mm from February 1975. 📊

REGIONAL PRECIPITATION AND ALERTS

● Coronel Suárez registers 204 mm with 118 mm between March 5 and March 6.

● Pigüé reaches 116 mm and Tres Arroyos reaches 119 mm.

● SMN issues successive alerts: yellow on March 5 and 6, orange on March 6 afternoon, and red on March 7 morning. 🚨

● The red level is confirmed after 07:00 on March 7 and downgraded later the same day.

● The SQPE-OBS system estimates 300 to 350 mm around Bahía Blanca during the peak interval.

● Sentinel-2 satellite data confirm increased surface water between February 9 and March 11. 🌿


INSTITUTIONAL FRAMEWORK

● The National Meteorological Service (SMN) provides institutional responsibility for monitoring and warnings in Argentina.

● The term “precipitable water” designates the vertically integrated mass of water vapor in an atmospheric column; etymologically, it derives from Latin “praecipitare” meaning “to cause to fall” and Old English “wæter.”

● The term “convective available potential energy” or CAPE denotes the integrated buoyant energy of an air parcel; etymologically, “convective” comes from Latin “convehere” meaning “to carry together,” “available” from Latin “ad” plus “habere” meaning “to have toward,” “potential” from Latin “potentia” meaning “power,” and “energy” from Greek “energeia.” 🔬

● The adjective “buoyant” specifies the ability of a parcel to rise when less dense than its environment; etymologically, it comes from Old French “buoy” meaning “float” and Late Latin “boia” meaning “fetter or float.”

● The term “recurrence period” identifies the statistical interval between extreme events; etymologically, “recurrence” originates from Latin “recurrere” meaning “to run back,” and “period” from Greek “periodos.”

● The term “satellite” denotes an artificial body orbiting Earth used for observation; etymologically, it comes from Latin “satelles” meaning “attendant.” 📡

● The institutional alert system uses a color code: yellow for potential risk, orange for high risk, and red for extreme risk.

● The magnitude of 312 mm in Bahía Blanca and 204 mm in Coronel Suárez are interpreted within this framework of statistical thresholds. 📘

● The official record of 150.9 mm in February 1975 demonstrates the historical basis for extreme rainfall comparison.

● The use of GOES-16 and Sentinel-2 establishes the technological dimension of institutional observation. 🛰️

● The etymology of “alert” derives from Italian “all’erta,” meaning “on the lookout,” and frames the preventive role of SMN communications.

● The combined interpretation of atmospheric dynamics and alert protocols reflects the integration of physical science with institutional governance.

● The SMN framework underscores that warnings complement but do not substitute broader disaster management strategies. 🏛️

Published by Leonardo Tomás Cardillo

https://www.linkedin.com/in/leonardocardillo

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