Presets and sharing
Inputs
Tidal events (up to 6 events)
| Type | Time (HH:MM) | Tide level (m) | Delete |
|---|
Tidal events are automatically sorted and displayed in chronological order.
Data acquisition (β)
Data acquisition (β) is regionally limited. If you cannot obtain it, please enter it manually.
Results
sunrise/sunset
- sunrise
- —
- sunset
- —
- photoperiod
- —
- condition
- —
Moon age/moon phase
- Moon phase
- —
- moon phase
- —
- Illuminance (approximate)
- —
Moon age/moon phase is estimated using the average lunar model.
Astronomy tools
Find related tools for sunrise, twilight, moon phase, and observing planning.
Tide (manual input)
| Type | time | Tide level (m) |
|---|
- Maximum tide level
- —
- minimum tide level
- —
- Tidal difference (maximum-minimum)
- —
The curve is not displayed because there are fewer than 2 tidal events.
Assumptions & limits
- Moon age/moon phase/illuminance are approximate estimates based on a simple model (lunar month 29.530588853 days).
- The tidal curve is a simple display that connects the extreme values of high tide and low tide using cosine interpolation.
- Actual tidal values vary depending on wind, atmospheric pressure, topography, river inflow, etc. Please be sure to check the official information.
How to use this calculator effectively
This guide helps you use Tide/moon phase/sunrise/sunset calculation in a repeatable way: define a baseline, change one variable at a time, and explain each output using explicit assumptions before sharing results.
How it works
The calculator applies deterministic formulas to your input values and only rounds at the final display layer. This makes it useful for comparative analysis: keep one scenario as a baseline, then vary assumptions and measure the delta in both absolute terms and percentage terms. If a change appears too large or too small, verify units, period conventions, and sign direction before interpreting the result.
When to use
Use this page when you need a fast planning estimate, a classroom check, or a reproducible scenario that teammates can review. It is most effective at the decision-prep stage, where you need to compare options quickly and decide which assumptions deserve deeper modeling or external validation.
Common mistakes to avoid
- Mixing units such as percent vs decimal, or monthly vs yearly settings.
- Changing multiple fields at once, which hides the real cause of result movement.
- Comparing outputs across tools without aligning constants and default conventions.
- Treating rounded display values as exact inputs for downstream calculations.
Interpretation and worked example
Start with a baseline case and save that output. Next, edit one assumption to reflect your realistic alternative, then compare both the direction and size of change. If the direction matches domain intuition and magnitude is plausible, your setup is likely coherent. If not, check hidden defaults, unit conversions, boundary conditions, and date logic before drawing conclusions.
See also
- Solar altitude, direction, sunrise/sunset, day length (ES-002)
- Distance to horizon / drop in earth curvature (refraction coefficient k) (ES-014)
- Distance and direction of two latitude and longitude points (great circle/ellipsoid) (ES-001)
- Tsunami wave speed/arrival time (shallow water wave c=√(gh)) (ES-008)
FAQ
Are the tide values accurate?
Since it is based on manual input or external forecast data, there may be differences from the actual tide level. Please be sure to follow official information and local warnings when making your final decision.
Why is the moon age different from other sites?
This tool uses a simple model. There may be differences from strict astronomical calculations.
What if data acquisition (β) cannot be used?
It may not be possible to obtain it due to regional restrictions or API restrictions. Please use the manual input mode by entering tidal events.
What should I enter first?
Start with the minimum required inputs shown above the calculate button, then keep optional settings at their defaults for a first pass. After getting a baseline, change one parameter at a time so you can explain which assumption moved the output.
How precise are the results?
The calculator keeps internal precision and rounds only for display. Small differences can still appear if another tool uses different constants, period conventions, or rounding rules. Align assumptions before comparing final values.
How to use Tide/moon phase/sunrise/sunset calculation effectively
What this calculator does
This page is for estimating outcomes by changing inputs in one controlled workflow. The model keeps your focus on variables, not output shape. Start with stable assumptions, then test sensitivity by changing one key input at a time to observe directional impact.
Input meaning and unit policy
Each input has an expected unit and a typical range. For reliable interpretation, check whether you are using the same unit system, period, and base assumptions across all runs. Unit mismatch is the most common source of unexpected drift in numeric results.
Use-case sequence
A practical sequence is: first run with defaults, then create a baseline log, then run one alternative scenario, and finally compare only the changed output metric. This sequence reduces cognitive load and prevents false pattern recognition in early experiments.
Common mistakes to avoid
Avoid changing too many variables at once, mixing incompatible data sources, and interpreting a one-time output without checking robustness. A single contradictory input can flip conclusions, so keep each experiment minimal and document assumptions as part of your note.
Interpretation guidance
Review both magnitude and direction. Direction tells you whether a strategy moves outcomes in the desired direction, while magnitude helps you judge practicality. If both agree, you can proceed; if not, rebuild the baseline and verify constraints before deciding.
Related tools
- Earth science/environment (atmosphere/weather (sun/humidity/air quality))
- Solar altitude, direction, sunrise/sunset, day length (ES-002)
- Distance to horizon / drop in earth curvature (refraction coefficient k) (ES-014)
- Distance and direction of two latitude and longitude points (great circle/ellipsoid) (ES-001)
- Tsunami wave speed/arrival time (shallow water wave c=√(gh)) (ES-008)