I’m trying to write a note that has steps 1, 2, 3, etc. The numbered list works except when I put an image or an information section using >[!info]. If I put something like that into step 3 (for example), step 4 becomes 1 instead of 4. How do I get add text on the next line without breaking the number sequence. For now, I have to use bullet points “- 1.”, - 2." which doesn’t look as clean as a simple numbered list.
Does manually renumbering the list work for you (just replace the 1 with whatever the sequential number should be and the list should continue thereafter)?
1. a list
2. another item
3. a third one
> [!NOTE] Title
> Contents
4. Fourth item
5. Fifth
6. sixth
## a heading
7. here is number 7
8. eight
9. nine
10. and ten
Unfortunately, no. Every time, I edit the number, say a 1 back to a 3, then hit enter to add the next item, 4, the number changes back to a 1. When I go to read mode, I have
“1.” this
“2.” that
picture or >[!info] text
“1.”
“2.”
frustrating but bullets with numbers - (1) work for now.
I had to add " " to get the text to show what I’m getting. I wish obsidian worked like this editor and keep the numbers in sequence.
Hi.
To paste raw text on the forum, put three backticks on the line above and the line below the block of text:
```
1. this
2. that
picture or >[!info] text
3. Three
4. Four
```
If you can share some sample raw code, someone might be able figure out a solution for you. It should work.
Thanks for your help!
###### Using the saturation mixing ratio is used in the context of calculating the CCL:
1. **Calculate Lifting Condensation Level (LCL):** [[Lifting Condensation Level (LCL)#^915ab8|Determine the LCL]] using the initial temperature and dew point temperature of the air parcel, along with the adiabatic lapse rate. This gives you the altitude at which the parcel becomes saturated as it rises.
2. **Determine Parcel's Mixing Ratio (w):** Calculate the mixing ratio (w) of the air parcel at the surface using the <span style="background:#fff88f"><u>actual</u> amount of water vapor present</span>. The mixing ratio represents the actual amount of water vapor in the air. To determine the mixing ratio (w) of a parcel of air, you'll need to know the mass of water vapor (in grams) present in the parcel and the mass of dry air (in kilograms) that the parcel contains.
>[!info] Determine the Mass of Water Vapor (m_v):
>Measure or calculate the mass of water vapor in the parcel. This can be obtained from humidity sensors, weather instruments, or calculated using dew point and temperature measurements.
> - Determine the Mass of Dry Air (m_d): Calculate the mass of the dry air in the parcel. The total mass of the parcel minus the mass of water vapor will give you the mass of dry air.
> - Calculate the Mixing Ratio (w): Divide the mass of water vapor (m_v) by the mass of dry air (m_d) and multiply by 1000 to convert to grams: >
> - Mixing Ratio (w) = (m_v / m_d) * 1000
> - The result will be the mixing ratio of the air parcel, expressed in grams of water vapor per kilogram of dry air.
> .
>- **For example,** if you have a parcel of air with 10 grams of water vapor and 1.2 kilograms of dry air, the mixing ratio would be calculated as:
>- Mixing Ratio (w) = (10 g / 1.2 kg) = 8.33 g/kg
>- This means that the air contains 8.33 grams of water vapor for every kilogram of dry air.
> .
>- **some approximate ranges for mixing ratios:**
> - **Very Dry Conditions**: In extremely dry regions like deserts, the mixing ratio can be as low as a few grams per kilogram (g/kg), often in the range of 1 to 5 g/kg. >
> - **Moderate Humidity**: In more temperate regions with moderate humidity, mixing ratios might range from about 5 to 15 g/kg.
> - **Higher Humidity:** In tropical and humid areas, mixing ratios can range from 15 to 25 g/kg or even higher.
> - **Convective Clouds:** Within convective clouds (which are actively rising and moistening), mixing ratios can increase significantly, sometimes exceeding 25 g/kg.
>
- 3. **Calculate Saturation Mixing Ratio (w__s_):** Determine the saturation mixing ratio (w__s_) based on the temperature of the air parcel at the surface. The saturation mixing ratio is the <span style="background:#fff88f"><u>maximum</u> amount of water vapor that the air can hold <u>at that temperature</u></span>.
>[!info] w_s = (e_s / p) * (R_d / R_v)
>Where:
> w_s is the saturation mixing ratio in grams of water vapor per kilogram of dry air.
> e_s is the saturation vapor pressure at the given temperature.
> p is the pressure of the air parcel.
> R_d is the specific gas constant for dry air (approximately 287.058 J/(kg·K)).
> R_v is the specific gas constant for water vapor (approximately 461.5 J/(kg·K)).
>[!info] e_s = 10^(A - B / (T + C)) is the Antoine equation relating the saturation vapor pressure of a substance to its temperature.
>Where:
> e_s is the saturation vapor pressure in millibars (mb) or hectopascals (hPa).
> T is the temperature in degrees Celsius.
> A, B, and C are constants specific to the substance. For water: A = 8.07131 B = 1730.63 C = 233.426
>
- 4. **Compare Mixing Ratios:** Compare the actual mixing ratio (w) of the air parcel with the saturation mixing ratio (w__s_). If w > w__s_ at the surface, it indicates that the air is already saturated or nearly saturated. This can suggest the potential for cloud formation even before the parcel reaches the CCL.
- 5. **Analyze CCL:** The Convective Condensation Level (CCL) is the altitude where the temperature of the rising air parcel matches the environmental temperature. If the actual mixing ratio (w) of the parcel exceeds the saturation mixing ratio (w__s_) at or below the CCL altitude, it suggests that cloud formation could occur as the air parcel rises to the CCL and condensation initiates.
Indent the callout to make it part of the preceding list item. See eightning’s post below — apparently callouts are a weird exception and you don’t indent them in this case like you would a normal blockquote or paragraph, unfortunately.
I’d also recommend putting spaces before and after it — it’s not always required but generally a good idea between to separate things in Markdown with blank lines.
Also, all of the > should have spaces after them.
3 Likes
Just type ctrl-z to undo the change each time it happens. The last change was the numbers changing, so your intentional change is preserved.
My version of the text (difficult to know what another user wants and will see because of the impact of different objectives, themes, and settings):
pdf.zip (84.1 KB)
###### Using the saturation mixing ratio is used in the context of calculating the CCL:
1. **Calculate Lifting Condensation Level (LCL):** [[Lifting Condensation Level (LCL)#^915ab8|Determine the LCL]] using the initial temperature and dew point temperature of the air parcel, along with the adiabatic lapse rate. This gives you the altitude at which the parcel becomes saturated as it rises.
2. **Determine Parcel's Mixing Ratio (w):** Calculate the mixing ratio (w) of the air parcel at the surface using the <span style="background:#fff88f"><u>actual</u> amount of water vapor present</span>. The mixing ratio represents the actual amount of water vapor in the air. To determine the mixing ratio (w) of a parcel of air, you'll need to know the mass of water vapor (in grams) present in the parcel and the mass of dry air (in kilograms) that the parcel contains.
> [!info] Determine the Mass of Water Vapor (m_v):
> Measure or calculate the mass of water vapor in the parcel. This can be obtained from humidity sensors, weather instruments, or calculated using dew point and temperature measurements.
> - Determine the Mass of Dry Air (m_d): Calculate the mass of the dry air in the parcel. The total mass of the parcel minus the mass of water vapor will give you the mass of dry air.
> - Calculate the Mixing Ratio (w): Divide the mass of water vapor (m_v) by the mass of dry air (m_d) and multiply by 1000 to convert to grams: >
> - Mixing Ratio (w) = (m_v / m_d) * 1000
> - The result will be the mixing ratio of the air parcel, expressed in grams of water vapor per kilogram of dry air.
> - **For example,** if you have a parcel of air with 10 grams of water vapor and 1.2 kilograms of dry air, the mixing ratio would be calculated as:
> - Mixing Ratio (w) = (10 g / 1.2 kg) = 8.33 g/kg
> - This means that the air contains 8.33 grams of water vapor for every kilogram of dry air.
> - **Some approximate ranges for mixing ratios:**
> - **Very Dry Conditions**: In extremely dry regions like deserts, the mixing ratio can be as low as a few grams per kilogram (g/kg), often in the range of 1 to 5 g/kg.
> - **Moderate Humidity**: In more temperate regions with moderate humidity, mixing ratios might range from about 5 to 15 g/kg.
> - **Higher Humidity:** In tropical and humid areas, mixing ratios can range from 15 to 25 g/kg or even higher.
> - **Convective Clouds:** Within convective clouds (which are actively rising and moistening), mixing ratios can increase significantly, sometimes exceeding 25 g/kg.
3. **Calculate Saturation Mixing Ratio (w__s_):** Determine the saturation mixing ratio (w__s_) based on the temperature of the air parcel at the surface. The saturation mixing ratio is the <span style="background:#fff88f"><u>maximum</u> amount of water vapor that the air can hold <u>at that temperature</u></span>.
> [!info] w_s = (e_s / p) * (R_d / R_v)
> - Where:
> - w_s is the saturation mixing ratio in grams of water vapor per kilogram of dry air.
> - e_s is the saturation vapor pressure at the given temperature.
> - p is the pressure of the air parcel.
> - R_d is the specific gas constant for dry air (approximately 287.058 J/(kg·K)).
> - R_v is the specific gas constant for water vapor (approximately 461.5 J/(kg·K)).
> [!info] e_s = 10^(A - B / (T + C)) is the Antoine equation relating the saturation vapor pressure of a substance to its temperature.
> - Where:
> - e_s is the saturation vapor pressure in millibars (mb) or hectopascals (hPa).
> - T is the temperature in degrees Celsius.
> - A, B, and C are constants specific to the substance. For water: A = 8.07131 B = 1730.63 C = 233.426
4. **Compare Mixing Ratios:** Compare the actual mixing ratio (w) of the air parcel with the saturation mixing ratio (w__s_). If w > w__s_ at the surface, it indicates that the air is already saturated or nearly saturated. This can suggest the potential for cloud formation even before the parcel reaches the CCL.
5. **Analyze CCL:** The Convective Condensation Level (CCL) is the altitude where the temperature of the rising air parcel matches the environmental temperature. If the actual mixing ratio (w) of the parcel exceeds the saturation mixing ratio (w__s_) at or below the CCL altitude, it suggests that cloud formation could occur as the air parcel rises to the CCL and condensation initiates.
6. Six
7. Seven
> [!NOTE] Title
> Contents
8. Eight
9. Nine
Gruber on using block elements in Markdown: