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Time:2025-12-17 13:38:14 Popularity:922
A hydrometeorological station restart does not automatically recover the rainfall or river-level history missed during an outage. First distinguish loss of the communication link from loss of sensor or logger power. A retained rainfall counter may preserve an interval total, while a restored level sensor reports the present water level, not the peak that occurred while it was unpowered.

A NiuBoL station can combine meteorological sensors, a rain gauge, a level instrument, acquisition equipment and remote communications. These elements do not necessarily share the same power circuit or storage function. A failed cellular connection can leave local measurement intact; a depleted station battery can stop both measurement and recording.
Before clearing alarms or resetting counters, record the last valid observation, the first available observation and any known equipment intervention. Inspect the logger's local history where the delivered configuration permits it. A gap in the remote chart alone does not establish whether the measurements are lost or waiting to be transferred.

| Outage condition | What may remain available | What must not be assumed |
|---|---|---|
| Backhaul unavailable; acquisition remains powered | Locally stored, time-stamped records if the configured logger retained them | Automatic backfill or unlimited retention without a demonstrated configuration |
| Pulse-counting logger loses power | Previously saved counts, subject to the logger's retention behavior | Tips occurring while the input was unpowered were counted |
| Separately powered digital rain gauge continues counting | A retained cumulative difference if the actual counter operates and does not reset | The timing of each tip or short-duration rainfall peaks can be reconstructed from that difference |
| Level sensor is unpowered | A new present-level measurement after valid operation resumes | The maximum or minimum level during the missing period is known |
| Clock or configuration changes during service | Records that can be interpreted with a dated change note | Upload order is the same as observation order |
Rainfall accumulation and instantaneous stage are different records. Their recovery rules should be specified separately. Filling every missing channel with zero would imply both no rainfall and a particular water level; neither conclusion follows from missing communications or power.

For the NiuBoL 0.5 mm tipping-bucket configuration, each valid measuring tip represents 0.5 mm. If a separately powered instrument retains a count that increases by 20 tips across a communications gap, the indicated accumulation is 10 mm. This illustrative recovery requires a continuous counter and a known coefficient; it is not a claim that every rain-gauge version stores counts independently.
Even a valid 10 mm difference says nothing about whether the rain fell steadily or in one short burst. Keep the total over its actual uncertain interval rather than assigning it all to the first restored minute. Where the logger's pulse input stopped counting, a later connection cannot recover pulses that were never recorded.
A radar level instrument measures distance to the water surface and the station converts that measurement using its installed reference. After power returns, confirm that the support, reference offset and target remain unchanged. A storm may damage the installation as well as interrupt its supply.

If a separate velocity or flow instrument is included, verify its own channels and calculation inputs. A restored water-level value does not recreate missing velocity or discharge. Any reconstruction or model estimate must remain distinguishable from direct observations, with its method and uncertainty identified by the responsible project team.
| Selected component | Relevant specification | Restart check |
|---|---|---|
| NBL-W-RS 0.5 mm rain gauge | 0.5 mm per tip; 0-4 mm/min; +/-4% under indoor static testing at 2 mm/min | Confirm coefficient, counting source and counter-reset behavior for the delivered output. |
| 77-79 GHz radar level configuration | Distance 0.15-65 m; 1 mm resolution; stated +/-1 mm at 4 m, 25 deg C and 40% RH; RS485 Modbus RTU | Recheck reference, target and valid measurement after restoration; do not infer missing extrema. |
| NBL-PH-1 data logger | RS485/RS232; configurable saving interval 1-240 minutes; onboard non-volatile storage | Verify actual retention, clock and transfer functions. The saving interval is not a guarantee of recovery from complete power loss. |

Compare the logger clock with the project's time convention before accepting recovered files. Record any correction made during service. A restarted clock, changed time zone or duplicated upload can create a misleading sequence even if the numerical measurements are correct.
Use station identity, channel and observation time when assessing duplicates, together with any sequence information actually provided. Do not use arrival time as the observation time merely because the platform received old records after reconnection. Preserve original records before attempting a controlled re-import.
Test delayed transfer with the receiving platform rather than assuming that a successful reconnection performs it. The NBL-PH-1 acquisition configuration and the receiving service must together support the required workflow. Confirm which recovery functions are included and which require operator action.

Perform separate, planned tests for backhaul interruption and acquisition power loss. Preserve settings and counters, and use a controlled rain-input test rather than waiting for a real storm. Confirm the last saved record, any lost interval, the first restored record and how the platform labels missing observations.
For a hydrometeorological station restart, also verify alarm recovery. A historical alarm should not disappear solely because the display now shows a normal value. Conversely, a retained old high reading must not be presented as a current event. The required behavior belongs to the project alarm design, not to the sensor's measurement range.

Only if the station acquired and retained the observations and the configured transfer workflow can deliver them. Confirm local storage and backfill separately. Reconnection cannot retrieve measurements that were never acquired while the station was unpowered.
It can recover a difference across the gap when the counter remained powered, retained its state and used the same coefficient. Check reset and rollover behavior. The difference does not recover the timing or intensity distribution within that interval.
No. It represents the water level when the valid observation resumed. A higher or lower level may have occurred during the gap. Keep that interval missing unless a separately identified reconstruction is available.
Record their values and understand the retention scheme first. An unnecessary reset can destroy the comparison needed to evaluate accumulation across a gap. Follow the approved service procedure and retain a dated reset note where resetting is required.
State which outage types must be covered, the required local retention, expected transfer workflow and missing-data presentation. Ask NiuBoL to identify sensor and logger responsibilities separately, then demonstrate the agreed recovery during acceptance.
A hydrometeorological station restart should restore valid monitoring without hiding the lost interval. Determine what continued measuring, preserve rain-counter state and distinguish current level from missing flood history. A tested recovery workflow makes NiuBoL station records easier to interpret after communications or power interruptions.
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