Welcome to Tides

Chris

Staff member
Welcome to the tides web app which has been serving the public since 2004.

When you register you can subscribe for member access. Members experience is without future date restrictions and without ads. Printing calendars for your reference or for your guests is available. The free service includes restrictions on the future content and is displayed with some ads.

Thank you for visiting. If you have a question about the site or your account and would like to speak with me, click on my name to start a conversation.


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An explanation of tides, for your reference.

Tides are primarily caused by the gravitational forces exerted by the Moon and, to a lesser extent, the Sun on Earth's oceans. Here's a step-by-step breakdown of how this works:

1. **Gravitational Pull:**
- **Moon's Influence:** The Moon exerts a gravitational pull on Earth, which is strongest on the side of Earth closest to the Moon. This pull causes water on Earth to bulge towards the Moon, creating a high tide.
- **Sun's Influence:** The Sun also pulls on Earth's water, but since it's much farther away than the Moon, its gravitational effect on tides is about half as strong. However, when the Sun, Moon, and Earth align (during new and full moons), their combined gravitational forces produce higher high tides, known as spring tides.

2. **Centrifugal Force:**
- As Earth rotates, there's also a centrifugal force (an apparent force due to the rotation) that tends to push water away from the center of rotation. This results in another bulge on the opposite side of Earth from the Moon, also contributing to high tide.

3. **Resulting Tides:**
- **High Tides:** There are typically two high tides daily because Earth rotates, bringing any given point on Earth under the Moon's gravitational bulge twice in about 24 hours and 50 minutes (the lunar day).
- **Low Tides:** Between these high tides, water levels drop, leading to low tides. This happens because water is drawn away to form the high tide bulges.

4. **Types of Tides:**
- **Spring Tides:** Occur when the Sun, Moon, and Earth are aligned, increasing the tidal range (the difference between high and low tide).
- **Neap Tides:** Happen when the Sun and Moon are at right angles to each other, reducing the tidal range because the gravitational forces partially cancel each other out.

5. **Local Factors:**
- The shape of the coastline, depth of the ocean, and local geography can greatly influence the timing and height of tides in any given area. For example, in narrow bays or inlets, tidal amplitude can be significantly amplified, leading to very high or low tides.

6. **Tidal Periodicity:**
- Tides have a semi-diurnal nature in most places, meaning two high and two low tides occur each day. However, some regions experience diurnal tides (one high and one low tide per day) or mixed tides where the pattern isn't as regular.

7. **Other Influences:**
- Weather conditions like wind, atmospheric pressure, and even earthquakes or tsunamis can temporarily alter tide levels.

In summary, tides result from the gravitational dance between Earth, the Moon, and the Sun, modulated by Earth's rotation and local geography. This interaction creates the rhythmic rise and fall of sea levels that we observe daily.
 
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Hi, Chris. I'm Brad. I would really like to join but, for the life of me, can't find any way to do it. I've been through several pages of Tides.net and cannot find a "Register" link.

Please advise,
Brad
 
Hi, Chris. I'm Brad. I would really like to join but, for the life of me, can't find any way to do it. I've been through several pages of Tides.net and cannot find a "Register" link.

Please advise,
Brad
Hi Brad, see attached…
B790B286-2E0E-49A0-861D-330164DED470.jpeg96486CE0-DD22-4C05-AE49-6984F2FA00A0.jpeg1675C9CE-4CDC-4BA6-8FDF-4069D3FD3D42.jpeg
 
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If I subscribe will I be allowed to use the Adobe PDF that I already have installed? Also can I download with Google Chrome?
 
If I subscribe will I be allowed to use the Adobe PDF that I already have installed? Also can I download with Google Chrome?
Yes with PDF, no with chrome for offline usage however it’s data and charts are cached well.
 
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Yes with PDF, no with chrome for offline usage however it’s data and charts are cached well.

Hey, Chris. my sub was renewed... but I can't see future tides still. Can you look into it?? Would appreciate it!

Paid through paypal.
Transaction ID
14V47923U24755624

Paid on 10/20.
 
Welcome to the tides web app which has been serving the public since 2004.

When you register you can subscribe for member access. Members experience is without future date restrictions and without ads. Printing calendars for your reference or for your guests is available. The free service includes restrictions on the future content and is displayed with some ads.

Thank you for visiting. If you have a question about the site or your account and would like to speak with me, click on my name to start a conversation.


View attachment 471View attachment 452View attachment 456View attachment 454View attachment 455 View attachment 473

An explanation of tides, for your reference.

Tides are primarily caused by the gravitational forces exerted by the Moon and, to a lesser extent, the Sun on Earth's oceans. Here's a step-by-step breakdown of how this works:

1. **Gravitational Pull:**
- **Moon's Influence:** The Moon exerts a gravitational pull on Earth, which is strongest on the side of Earth closest to the Moon. This pull causes water on Earth to bulge towards the Moon, creating a high tide.
- **Sun's Influence:** The Sun also pulls on Earth's water, but since it's much farther away than the Moon, its gravitational effect on tides is about half as strong. However, when the Sun, Moon, and Earth align (during new and full moons), their combined gravitational forces produce higher high tides, known as spring tides.

2. **Centrifugal Force:**
- As Earth rotates, there's also a centrifugal force (an apparent force due to the rotation) that tends to push water away from the center of rotation. This results in another bulge on the opposite side of Earth from the Moon, also contributing to high tide.

3. **Resulting Tides:**
- **High Tides:** There are typically two high tides daily because Earth rotates, bringing any given point on Earth under the Moon's gravitational bulge twice in about 24 hours and 50 minutes (the lunar day).
- **Low Tides:** Between these high tides, water levels drop, leading to low tides. This happens because water is drawn away to form the high tide bulges.

4. **Types of Tides:**
- **Spring Tides:** Occur when the Sun, Moon, and Earth are aligned, increasing the tidal range (the difference between high and low tide).
- **Neap Tides:** Happen when the Sun and Moon are at right angles to each other, reducing the tidal range because the gravitational forces partially cancel each other out.

5. **Local Factors:**
- The shape of the coastline, depth of the ocean, and local geography can greatly influence the timing and height of tides in any given area. For example, in narrow bays or inlets, tidal amplitude can be significantly amplified, leading to very high or low tides.

6. **Tidal Periodicity:**
- Tides have a semi-diurnal nature in most places, meaning two high and two low tides occur each day. However, some regions experience diurnal tides (one high and one low tide per day) or mixed tides where the pattern isn't as regular.

7. **Other Influences:**
- Weather conditions like wind, atmospheric pressure, and even earthquakes or tsunamis can temporarily alter tide levels.

In summary, tides result from the gravitational dance between Earth, the Moon, and the Sun, modulated by Earth's rotation and local geography. This interaction creates the rhythmic rise and fall of sea levels that we observe daily.
Hey Chris - I have noticed that when looking at the Jan 25 table for a specific location and click on Tide Tables in column format, it works. But if I am looking at the Feb chart (or any other month) and click on Tide Tables column format, it goes back to January. How do I get future month tide tables in column format? Apologies if I am missing something. Thanks.
 
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