Oslava at Dolní Bory-Olší
The Oslava at Dolní Bory-Olší read 28 cm at .
Last updated . This page normally updates every hour; the latest update is late.
28 cmProvisional
- Change in a day
- +6 cm
Where the water stands
That is below the first flood activity degree (vigilance) of 80 cm set by the Czech Hydrometeorological Institute.
Table: where the water stands
| Level | Value |
|---|---|
| Newest reading | 28 cm, |
| Hydrological drought level | 4 cm |
| First flood activity degree (vigilance) | 80 cm |
| Second flood activity degree (readiness) | 110 cm |
| Third flood activity degree (danger) | 130 cm |
| Extreme flood level | 195 cm |
The last 90 days
- Level
Table: The last 90 days
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About these figures
Official levels
- Hydrological drought level: 4 cm. (hydrologické sucho) The newest reading is 24 cm above it.Set by Zdroj: Český hydrometeorologický ústav (CHMI), CC BY 4.0.
- First flood activity degree (vigilance): 80 cm. (stav bdělosti) The newest reading is 52 cm below it.Set by Zdroj: Český hydrometeorologický ústav (CHMI), CC BY 4.0.
- Second flood activity degree (readiness): 110 cm. (stav pohotovosti) The newest reading is 82 cm below it.Set by Zdroj: Český hydrometeorologický ústav (CHMI), CC BY 4.0.
- Third flood activity degree (danger): 130 cm. (stav ohrožení) The newest reading is 102 cm below it.Set by Zdroj: Český hydrometeorologický ústav (CHMI), CC BY 4.0.
- Extreme flood level: 195 cm. (extrémní povodeň) The newest reading is 167 cm below it.Set by Zdroj: Český hydrometeorologický ústav (CHMI), CC BY 4.0.
About this gauge
Dolní Bory-Olší is a gauge on the Oslava in Czechia.
It lies at 49.4225° N, 15.9855° E.
Its readings come from the Czech Hydrometeorological Institute (CHMI).
The gauge reads the height of the water above a fixed zero, not the depth of the river.
Readings since 1 January 2026: too short a record for a normal range for the date or for records that mean much.
CHMI publishes its 10-minute readings as current data that it has not validated yet.
The newest reading is provisional: the source may still correct it.