Svatava at Kraslice
The Svatava at Kraslice read 11 cm at .
Last updated . This page normally updates every hour; the latest update is late.
11 cmProvisional
- Change in a day
- +3 cm
Where the water stands
That is below the first flood activity degree (vigilance) of 94 cm set by the Czech Hydrometeorological Institute.
Table: where the water stands
| Level | Value |
|---|---|
| Newest reading | 11 cm, |
| Hydrological drought level | 8 cm |
| First flood activity degree (vigilance) | 94 cm |
| Second flood activity degree (readiness) | 119 cm |
| Third flood activity degree (danger) | 139 cm |
| Extreme flood level | 169 cm |
The last 90 days
- Level
- Official level
Table: The last 90 days
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About these figures
Official levels
- Hydrological drought level: 8 cm. (hydrologické sucho) The newest reading is 3 cm above it.Set by Zdroj: Český hydrometeorologický ústav (CHMI), CC BY 4.0.
- First flood activity degree (vigilance): 94 cm. (stav bdělosti) The newest reading is 83 cm below it.Set by Zdroj: Český hydrometeorologický ústav (CHMI), CC BY 4.0.
- Second flood activity degree (readiness): 119 cm. (stav pohotovosti) The newest reading is 108 cm below it.Set by Zdroj: Český hydrometeorologický ústav (CHMI), CC BY 4.0.
- Third flood activity degree (danger): 139 cm. (stav ohrožení) The newest reading is 128 cm below it.Set by Zdroj: Český hydrometeorologický ústav (CHMI), CC BY 4.0.
- Extreme flood level: 169 cm. (extrémní povodeň) The newest reading is 158 cm below it.Set by Zdroj: Český hydrometeorologický ústav (CHMI), CC BY 4.0.
About this gauge
Kraslice is a gauge on the Svatava in Czechia.
It lies at 50.3163° N, 12.5185° 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.