From e424d96f573875e8e0e2418b211701e57f491a15 Mon Sep 17 00:00:00 2001 From: cyschneck <22159116+cyschneck@users.noreply.github.com> Date: Mon, 6 Jan 2025 15:53:13 -0700 Subject: [PATCH 1/9] fao equations --- ncl/ncl_entries/meteorology.ipynb | 28 ++++++++++++++++++++++++---- 1 file changed, 24 insertions(+), 4 deletions(-) diff --git a/ncl/ncl_entries/meteorology.ipynb b/ncl/ncl_entries/meteorology.ipynb index 5837d9a3..9488a63d 100644 --- a/ncl/ncl_entries/meteorology.ipynb +++ b/ncl/ncl_entries/meteorology.ipynb @@ -78,7 +78,15 @@ "source": [ "## daylight_fao56\n", "\n", - "NCL's `daylight_fao56` calculates the maximum number of daylight hours as described in the Food and Agriculture Organization (FAO) Irrigation and Drainage Paper 56 [(Chapter 3, Equation 34)](https://www.fao.org/4/X0490E/x0490e07.htm#chapter%203%20%20%20meteorological%20data) {footcite}`allan_fao_1998`" + "NCL's `daylight_fao56` calculates the maximum number of daylight hours as described in the Food and Agriculture Organization (FAO) Irrigation and Drainage Paper 56 [(Chapter 3, Equation 34)](https://www.fao.org/4/X0490E/x0490e07.htm#chapter%203%20%20%20meteorological%20data) {footcite}`allan_fao_1998`\n", + "\n", + "Where the maximum number of daylight hours, N, is calulated as:\n", + "\n", + "{math}`{\\omega}_{s} = arccos[-tan({\\phi})tan({\\delta})]`\n", + "\n", + "Where {math}`{\\omega}_{s}` is the sunset hour angle in radians [(Chapter 3, Eqution 25)](https://www.fao.org/4/X0490E/x0490e07.htm#chapter%203%20%20%20meteorological%20data) {footcite}`allan_fao_1998`\n", + "\n", + "{math}`N = \\frac{24}{{\\pi}} {\\omega}_{s}`" ] }, { @@ -125,7 +133,11 @@ "source": [ "## satvpr_temp_fao56\n", "\n", - "NCL's `satvpr_temp_fao56` calculates saturation vapor pressure using temperature as described in the Food and Agriculture Organization (FAO) Irrigation and Drainage Paper 56 [(Chapter 3, Equation 11)](https://www.fao.org/4/x0490e/x0490e07.htm) {footcite}`allan_fao_1998`" + "NCL's `satvpr_temp_fao56` calculates saturation vapor pressure using temperature as described in the Food and Agriculture Organization (FAO) Irrigation and Drainage Paper 56 [(Chapter 3, Equation 11)](https://www.fao.org/4/x0490e/x0490e07.htm) {footcite}`allan_fao_1998`\n", + "\n", + "Where the saturation vapor pressure, {math}`e^°` (kPa), at air temperature {math}`T` (°C) is calculated as:\n", + "\n", + "{math}`e^°(T) = 0.6108 {\\exp}[\\frac{17.27T}{T + 237.3}]`" ] }, { @@ -169,7 +181,11 @@ "source": [ "## satvpr_tdew_fao56\n", "\n", - "NCL's `satvpr_tdew_fao56` calculates the actual saturation vapor pressure using dewpoint temperature as described in the Food and Agriculture Organization (FAO) Irrigation and Drainage Paper 56 [(Chapter 3, Equation 14)](https://www.fao.org/4/x0490e/x0490e07.htm) {footcite}`allan_fao_1998`" + "NCL's `satvpr_tdew_fao56` calculates the actual saturation vapor pressure using dewpoint temperature as described in the Food and Agriculture Organization (FAO) Irrigation and Drainage Paper 56 [(Chapter 3, Equation 14)](https://www.fao.org/4/x0490e/x0490e07.htm) {footcite}`allan_fao_1998`\n", + "\n", + "Where the actual vapor pressure, {math}`e_{a}` (kPa), is saturation vapor presssure at a specific dewpoint temperature, {math}`T_{dew}` (°C) which is calculated as:\n", + "\n", + "{math}`e_{a} = e^°(T_{dew}) = 0.6108 {\\exp}[\\frac{17.27 T_{dew}}{T_{dew} + 237.3}]`" ] }, { @@ -206,7 +222,11 @@ "source": [ "## satvpr_slope_fao56\n", "\n", - "NCL's `satvpr_slope_fao56` calculates the slope of the saturation vapor pressure curve as described in the Food and Agriculture Organization (FAO) Irrigation and Drainage Paper 56 [(Chapter 3, Equation 13)](https://www.fao.org/4/x0490e/x0490e07.htm) {footcite}`allan_fao_1998`" + "NCL's `satvpr_slope_fao56` calculates the slope of the saturation vapor pressure curve as described in the Food and Agriculture Organization (FAO) Irrigation and Drainage Paper 56 [(Chapter 3, Equation 13)](https://www.fao.org/4/x0490e/x0490e07.htm) {footcite}`allan_fao_1998`\n", + "\n", + "Where the slope of saturation vapor pressure curve, {math}`{\\Delta}` (kPa), at air temperature {math}`T` (°C) is calculated as:\n", + "\n", + "{math}`{\\Delta} = \\frac{4098 [0.6108 {\\exp}[\\frac{17.27T}{T + 237.3}]}{(T + 237.3)^2}`" ] }, { From 4abb3dcde19521d6dfef0d5033adf5975c03bfa6 Mon Sep 17 00:00:00 2001 From: cyschneck <22159116+cyschneck@users.noreply.github.com> Date: Mon, 6 Jan 2025 15:57:45 -0700 Subject: [PATCH 2/9] fix spelling --- ncl/ncl_entries/meteorology.ipynb | 6 +++--- 1 file changed, 3 insertions(+), 3 deletions(-) diff --git a/ncl/ncl_entries/meteorology.ipynb b/ncl/ncl_entries/meteorology.ipynb index 9488a63d..2b038be6 100644 --- a/ncl/ncl_entries/meteorology.ipynb +++ b/ncl/ncl_entries/meteorology.ipynb @@ -80,11 +80,11 @@ "\n", "NCL's `daylight_fao56` calculates the maximum number of daylight hours as described in the Food and Agriculture Organization (FAO) Irrigation and Drainage Paper 56 [(Chapter 3, Equation 34)](https://www.fao.org/4/X0490E/x0490e07.htm#chapter%203%20%20%20meteorological%20data) {footcite}`allan_fao_1998`\n", "\n", - "Where the maximum number of daylight hours, N, is calulated as:\n", + "Where the maximum number of daylight hours, N, is calculated as:\n", "\n", "{math}`{\\omega}_{s} = arccos[-tan({\\phi})tan({\\delta})]`\n", "\n", - "Where {math}`{\\omega}_{s}` is the sunset hour angle in radians [(Chapter 3, Eqution 25)](https://www.fao.org/4/X0490E/x0490e07.htm#chapter%203%20%20%20meteorological%20data) {footcite}`allan_fao_1998`\n", + "Where {math}`{\\omega}_{s}` is the sunset hour angle in radians [(Chapter 3, Equation 25)](https://www.fao.org/4/X0490E/x0490e07.htm#chapter%203%20%20%20meteorological%20data) {footcite}`allan_fao_1998`\n", "\n", "{math}`N = \\frac{24}{{\\pi}} {\\omega}_{s}`" ] @@ -183,7 +183,7 @@ "\n", "NCL's `satvpr_tdew_fao56` calculates the actual saturation vapor pressure using dewpoint temperature as described in the Food and Agriculture Organization (FAO) Irrigation and Drainage Paper 56 [(Chapter 3, Equation 14)](https://www.fao.org/4/x0490e/x0490e07.htm) {footcite}`allan_fao_1998`\n", "\n", - "Where the actual vapor pressure, {math}`e_{a}` (kPa), is saturation vapor presssure at a specific dewpoint temperature, {math}`T_{dew}` (°C) which is calculated as:\n", + "Where the actual vapor pressure, {math}`e_{a}` (kPa), is saturation vapor pressure at a specific dewpoint temperature, {math}`T_{dew}` (°C) which is calculated as:\n", "\n", "{math}`e_{a} = e^°(T_{dew}) = 0.6108 {\\exp}[\\frac{17.27 T_{dew}}{T_{dew} + 237.3}]`" ] From 09c072561441905c7bef64dbd4293382fece528b Mon Sep 17 00:00:00 2001 From: cyschneck <22159116+cyschneck@users.noreply.github.com> Date: Mon, 6 Jan 2025 16:20:13 -0700 Subject: [PATCH 3/9] update edits --- ncl/ncl_entries/meteorology.ipynb | 10 +++++----- 1 file changed, 5 insertions(+), 5 deletions(-) diff --git a/ncl/ncl_entries/meteorology.ipynb b/ncl/ncl_entries/meteorology.ipynb index 2b038be6..dd576fdf 100644 --- a/ncl/ncl_entries/meteorology.ipynb +++ b/ncl/ncl_entries/meteorology.ipynb @@ -82,11 +82,11 @@ "\n", "Where the maximum number of daylight hours, N, is calculated as:\n", "\n", - "{math}`{\\omega}_{s} = arccos[-tan({\\phi})tan({\\delta})]`\n", + "{math}`N = \\frac{24}{{\\pi}} {\\omega}_{s}`\n", "\n", "Where {math}`{\\omega}_{s}` is the sunset hour angle in radians [(Chapter 3, Equation 25)](https://www.fao.org/4/X0490E/x0490e07.htm#chapter%203%20%20%20meteorological%20data) {footcite}`allan_fao_1998`\n", "\n", - "{math}`N = \\frac{24}{{\\pi}} {\\omega}_{s}`" + "{math}`{\\omega}_{s} = arccos[-tan({\\phi})tan({\\delta})]`" ] }, { @@ -135,7 +135,7 @@ "\n", "NCL's `satvpr_temp_fao56` calculates saturation vapor pressure using temperature as described in the Food and Agriculture Organization (FAO) Irrigation and Drainage Paper 56 [(Chapter 3, Equation 11)](https://www.fao.org/4/x0490e/x0490e07.htm) {footcite}`allan_fao_1998`\n", "\n", - "Where the saturation vapor pressure, {math}`e^°` (kPa), at air temperature {math}`T` (°C) is calculated as:\n", + "Where the saturation vapor pressure, {math}`e^°` (kPa), at air temperature, {math}`T` (°C), is calculated as:\n", "\n", "{math}`e^°(T) = 0.6108 {\\exp}[\\frac{17.27T}{T + 237.3}]`" ] @@ -183,7 +183,7 @@ "\n", "NCL's `satvpr_tdew_fao56` calculates the actual saturation vapor pressure using dewpoint temperature as described in the Food and Agriculture Organization (FAO) Irrigation and Drainage Paper 56 [(Chapter 3, Equation 14)](https://www.fao.org/4/x0490e/x0490e07.htm) {footcite}`allan_fao_1998`\n", "\n", - "Where the actual vapor pressure, {math}`e_{a}` (kPa), is saturation vapor pressure at a specific dewpoint temperature, {math}`T_{dew}` (°C) which is calculated as:\n", + "Where the actual vapor pressure, {math}`e_{a}` (kPa), is saturation vapor pressure at a specific dewpoint temperature, {math}`T_{dew}` (°C), which is calculated as:\n", "\n", "{math}`e_{a} = e^°(T_{dew}) = 0.6108 {\\exp}[\\frac{17.27 T_{dew}}{T_{dew} + 237.3}]`" ] @@ -226,7 +226,7 @@ "\n", "Where the slope of saturation vapor pressure curve, {math}`{\\Delta}` (kPa), at air temperature {math}`T` (°C) is calculated as:\n", "\n", - "{math}`{\\Delta} = \\frac{4098 [0.6108 {\\exp}[\\frac{17.27T}{T + 237.3}]}{(T + 237.3)^2}`" + "{math}`{\\Delta} = \\frac{4098 (0.6108 {\\exp}[\\frac{17.27T}{T + 237.3}])}{(T + 237.3)^2}`" ] }, { From 881372c9b8a166e6289acb08460c991abef3678c Mon Sep 17 00:00:00 2001 From: cyschneck <22159116+cyschneck@users.noreply.github.com> Date: Wed, 8 Jan 2025 16:00:04 -0700 Subject: [PATCH 4/9] sunrise equation --- ncl/ncl_entries/meteorology.ipynb | 2 +- 1 file changed, 1 insertion(+), 1 deletion(-) diff --git a/ncl/ncl_entries/meteorology.ipynb b/ncl/ncl_entries/meteorology.ipynb index dd576fdf..0b2782cf 100644 --- a/ncl/ncl_entries/meteorology.ipynb +++ b/ncl/ncl_entries/meteorology.ipynb @@ -84,7 +84,7 @@ "\n", "{math}`N = \\frac{24}{{\\pi}} {\\omega}_{s}`\n", "\n", - "Where {math}`{\\omega}_{s}` is the sunset hour angle in radians [(Chapter 3, Equation 25)](https://www.fao.org/4/X0490E/x0490e07.htm#chapter%203%20%20%20meteorological%20data) {footcite}`allan_fao_1998`\n", + "Where {math}`{\\omega}_{s}` is the sunset hour angle in radians [(Chapter 3, Equation 25)](https://www.fao.org/4/X0490E/x0490e07.htm#chapter%203%20%20%20meteorological%20data) {footcite}`allan_fao_1998` which is calculated from the latitude of the observer on Earth ({math}`\\phi`) and the sun's declination ({math}`\\delta`):\n", "\n", "{math}`{\\omega}_{s} = arccos[-tan({\\phi})tan({\\delta})]`" ] From a759344adcc5431cee4a4ed0c9b27fa2822c15a7 Mon Sep 17 00:00:00 2001 From: cyschneck <22159116+cyschneck@users.noreply.github.com> Date: Mon, 13 Jan 2025 15:32:32 -0700 Subject: [PATCH 5/9] dew point temp --- ncl/ncl_entries/meteorology.ipynb | 8 ++++++++ 1 file changed, 8 insertions(+) diff --git a/ncl/ncl_entries/meteorology.ipynb b/ncl/ncl_entries/meteorology.ipynb index 0b2782cf..0bb55f58 100644 --- a/ncl/ncl_entries/meteorology.ipynb +++ b/ncl/ncl_entries/meteorology.ipynb @@ -29,6 +29,14 @@ "## dewtemp_trh\n", "NCL's `dewtemp_trh` calculates the dew point temperature given temperature and relative humidity using the equations from John Dutton's _\"Ceaseless Wind\"_ (pg. 273-274){footcite}`dutton_1986` and returns a temperature in Kelvin\n", "\n", + "For the gas constant for water vapor of 461.5 {math}`\\frac{J}{K*kg}` ({math}`\\frac{461.5}{1000 * 4.186} \\frac{cal}{g*k}`) and the empirical value of the latent heat is (pg. 273, Problem 8.3.1):\n", + "\n", + "{math}`L_{lv} = 597.3 - 0.57(T - 273)`\n", + "\n", + "Then, where {math}`h` is the relative humidity and {math}`R_{v}` is the gas constant of water vapor, the dew point temperature (solved for as {math}`T_D`) (pg. 273, Equation 6) is:\n", + "\n", + "{math}`T_D = \\frac{T * L_{lv}}{L_{lv} - R_{v}Tlog(h)}`\n", + "\n", "
\n", "

Important Note

\n", " To convert from Kelvin to Celsius -273.15 and to convert from Celsius to Kelvin +273.15\n", From 2b092550d79a8a2cfbd2d0f9e7ab2c3eae653a9e Mon Sep 17 00:00:00 2001 From: cyschneck <22159116+cyschneck@users.noreply.github.com> Date: Mon, 13 Jan 2025 15:39:00 -0700 Subject: [PATCH 6/9] edits to wording --- ncl/ncl_entries/meteorology.ipynb | 6 +++--- 1 file changed, 3 insertions(+), 3 deletions(-) diff --git a/ncl/ncl_entries/meteorology.ipynb b/ncl/ncl_entries/meteorology.ipynb index 0bb55f58..c70ce723 100644 --- a/ncl/ncl_entries/meteorology.ipynb +++ b/ncl/ncl_entries/meteorology.ipynb @@ -27,13 +27,13 @@ "metadata": {}, "source": [ "## dewtemp_trh\n", - "NCL's `dewtemp_trh` calculates the dew point temperature given temperature and relative humidity using the equations from John Dutton's _\"Ceaseless Wind\"_ (pg. 273-274){footcite}`dutton_1986` and returns a temperature in Kelvin\n", + "NCL's `dewtemp_trh` calculates the dew point temperature given temperature and relative humidity using the equations from John Dutton's _\"Ceaseless Wind\"_ (pg. 273-274){footcite}`dutton_1986` and returns a temperature in Kelvin.\n", "\n", - "For the gas constant for water vapor of 461.5 {math}`\\frac{J}{K*kg}` ({math}`\\frac{461.5}{1000 * 4.186} \\frac{cal}{g*k}`) and the empirical value of the latent heat is (pg. 273, Problem 8.3.1):\n", + "Where, for a gas constant for water vapor ({math}`R_{v}`)of 461.5 {math}`\\frac{J}{K*kg}` ({math}`\\frac{461.5}{1000 * 4.186} \\frac{cal}{g*k}`) and the empirical value of the latent heat (pg. 273, Problem 8.3.1) is:\n", "\n", "{math}`L_{lv} = 597.3 - 0.57(T - 273)`\n", "\n", - "Then, where {math}`h` is the relative humidity and {math}`R_{v}` is the gas constant of water vapor, the dew point temperature (solved for as {math}`T_D`) (pg. 273, Equation 6) is:\n", + "So, when {math}`h` is the relative humidity, the dew point temperature (solved for as {math}`T_D`) (pg. 273, Equation 6) is:\n", "\n", "{math}`T_D = \\frac{T * L_{lv}}{L_{lv} - R_{v}Tlog(h)}`\n", "\n", From 24fabfd2831217ef8581d77a0ae1d2c1c9bb776e Mon Sep 17 00:00:00 2001 From: cyschneck <22159116+cyschneck@users.noreply.github.com> Date: Tue, 14 Jan 2025 12:44:41 -0700 Subject: [PATCH 7/9] edits --- ncl/ncl_entries/meteorology.ipynb | 4 ++-- 1 file changed, 2 insertions(+), 2 deletions(-) diff --git a/ncl/ncl_entries/meteorology.ipynb b/ncl/ncl_entries/meteorology.ipynb index c70ce723..b1d85095 100644 --- a/ncl/ncl_entries/meteorology.ipynb +++ b/ncl/ncl_entries/meteorology.ipynb @@ -29,11 +29,11 @@ "## dewtemp_trh\n", "NCL's `dewtemp_trh` calculates the dew point temperature given temperature and relative humidity using the equations from John Dutton's _\"Ceaseless Wind\"_ (pg. 273-274){footcite}`dutton_1986` and returns a temperature in Kelvin.\n", "\n", - "Where, for a gas constant for water vapor ({math}`R_{v}`)of 461.5 {math}`\\frac{J}{K*kg}` ({math}`\\frac{461.5}{1000 * 4.186} \\frac{cal}{g*k}`) and the empirical value of the latent heat (pg. 273, Problem 8.3.1) is:\n", + "Where, for the gas constant of water vapor ({math}`R_{v}`)of 461.5 {math}`\\frac{J}{K*kg}` ({math}`\\frac{461.5}{1000 * 4.186} \\frac{cal}{g*k}`), the empirical value of the latent heat (pg. 273, Problem 8.3.1) is:\n", "\n", "{math}`L_{lv} = 597.3 - 0.57(T - 273)`\n", "\n", - "So, when {math}`h` is the relative humidity, the dew point temperature (solved for as {math}`T_D`) (pg. 273, Equation 6) is:\n", + "So, when {math}`h` is the relative humidity, the dew point temperature (pg. 273, Equation 6, solved for as {math}`T_D`) is:\n", "\n", "{math}`T_D = \\frac{T * L_{lv}}{L_{lv} - R_{v}Tlog(h)}`\n", "\n", From 58f2cb583a41eee48df7cf79dd79721a179c51d9 Mon Sep 17 00:00:00 2001 From: cyschneck <22159116+cyschneck@users.noreply.github.com> Date: Tue, 14 Jan 2025 13:19:40 -0700 Subject: [PATCH 8/9] wording edits --- ncl/ncl_entries/meteorology.ipynb | 14 +++++++------- 1 file changed, 7 insertions(+), 7 deletions(-) diff --git a/ncl/ncl_entries/meteorology.ipynb b/ncl/ncl_entries/meteorology.ipynb index b1d85095..5365c845 100644 --- a/ncl/ncl_entries/meteorology.ipynb +++ b/ncl/ncl_entries/meteorology.ipynb @@ -86,13 +86,13 @@ "source": [ "## daylight_fao56\n", "\n", - "NCL's `daylight_fao56` calculates the maximum number of daylight hours as described in the Food and Agriculture Organization (FAO) Irrigation and Drainage Paper 56 [(Chapter 3, Equation 34)](https://www.fao.org/4/X0490E/x0490e07.htm#chapter%203%20%20%20meteorological%20data) {footcite}`allan_fao_1998`\n", + "NCL's `daylight_fao56` calculates the maximum number of daylight hours as described in the Food and Agriculture Organization (FAO) Irrigation and Drainage Paper 56 [(Chapter 3, Equation 34)](https://www.fao.org/4/X0490E/x0490e07.htm#chapter%203%20%20%20meteorological%20data) {footcite}`allan_fao_1998`.\n", "\n", - "Where the maximum number of daylight hours, N, is calculated as:\n", + "Where the maximum number of daylight hours, {math}`N`:\n", "\n", "{math}`N = \\frac{24}{{\\pi}} {\\omega}_{s}`\n", "\n", - "Where {math}`{\\omega}_{s}` is the sunset hour angle in radians [(Chapter 3, Equation 25)](https://www.fao.org/4/X0490E/x0490e07.htm#chapter%203%20%20%20meteorological%20data) {footcite}`allan_fao_1998` which is calculated from the latitude of the observer on Earth ({math}`\\phi`) and the sun's declination ({math}`\\delta`):\n", + "And {math}`{\\omega}_{s}` is the sunset hour angle in radians [(Chapter 3, Equation 25)](https://www.fao.org/4/X0490E/x0490e07.htm#chapter%203%20%20%20meteorological%20data) {footcite}`allan_fao_1998` which is calculated from the latitude of the observer on Earth ({math}`\\phi`) and the sun's declination ({math}`\\delta`):\n", "\n", "{math}`{\\omega}_{s} = arccos[-tan({\\phi})tan({\\delta})]`" ] @@ -141,9 +141,9 @@ "source": [ "## satvpr_temp_fao56\n", "\n", - "NCL's `satvpr_temp_fao56` calculates saturation vapor pressure using temperature as described in the Food and Agriculture Organization (FAO) Irrigation and Drainage Paper 56 [(Chapter 3, Equation 11)](https://www.fao.org/4/x0490e/x0490e07.htm) {footcite}`allan_fao_1998`\n", + "NCL's `satvpr_temp_fao56` calculates saturation vapor pressure using temperature as described in the Food and Agriculture Organization (FAO) Irrigation and Drainage Paper 56 [(Chapter 3, Equation 11)](https://www.fao.org/4/x0490e/x0490e07.htm) {footcite}`allan_fao_1998`.\n", "\n", - "Where the saturation vapor pressure, {math}`e^°` (kPa), at air temperature, {math}`T` (°C), is calculated as:\n", + "Where the saturation vapor pressure, {math}`e^°` (kPa), at air temperature {math}`T` (°C) is calculated as:\n", "\n", "{math}`e^°(T) = 0.6108 {\\exp}[\\frac{17.27T}{T + 237.3}]`" ] @@ -189,7 +189,7 @@ "source": [ "## satvpr_tdew_fao56\n", "\n", - "NCL's `satvpr_tdew_fao56` calculates the actual saturation vapor pressure using dewpoint temperature as described in the Food and Agriculture Organization (FAO) Irrigation and Drainage Paper 56 [(Chapter 3, Equation 14)](https://www.fao.org/4/x0490e/x0490e07.htm) {footcite}`allan_fao_1998`\n", + "NCL's `satvpr_tdew_fao56` calculates the actual saturation vapor pressure using dewpoint temperature as described in the Food and Agriculture Organization (FAO) Irrigation and Drainage Paper 56 [(Chapter 3, Equation 14)](https://www.fao.org/4/x0490e/x0490e07.htm) {footcite}`allan_fao_1998`.\n", "\n", "Where the actual vapor pressure, {math}`e_{a}` (kPa), is saturation vapor pressure at a specific dewpoint temperature, {math}`T_{dew}` (°C), which is calculated as:\n", "\n", @@ -230,7 +230,7 @@ "source": [ "## satvpr_slope_fao56\n", "\n", - "NCL's `satvpr_slope_fao56` calculates the slope of the saturation vapor pressure curve as described in the Food and Agriculture Organization (FAO) Irrigation and Drainage Paper 56 [(Chapter 3, Equation 13)](https://www.fao.org/4/x0490e/x0490e07.htm) {footcite}`allan_fao_1998`\n", + "NCL's `satvpr_slope_fao56` calculates the slope of the saturation vapor pressure curve as described in the Food and Agriculture Organization (FAO) Irrigation and Drainage Paper 56 [(Chapter 3, Equation 13)](https://www.fao.org/4/x0490e/x0490e07.htm) {footcite}`allan_fao_1998`.\n", "\n", "Where the slope of saturation vapor pressure curve, {math}`{\\Delta}` (kPa), at air temperature {math}`T` (°C) is calculated as:\n", "\n", From 2dc08afa2e8efe5a1cbb1e67b2d4f8889b044554 Mon Sep 17 00:00:00 2001 From: cyschneck <22159116+cyschneck@users.noreply.github.com> Date: Tue, 14 Jan 2025 13:29:10 -0700 Subject: [PATCH 9/9] clear ouputs --- ncl/ncl_entries/meteorology.ipynb | 2 +- 1 file changed, 1 insertion(+), 1 deletion(-) diff --git a/ncl/ncl_entries/meteorology.ipynb b/ncl/ncl_entries/meteorology.ipynb index 5365c845..17663c5f 100644 --- a/ncl/ncl_entries/meteorology.ipynb +++ b/ncl/ncl_entries/meteorology.ipynb @@ -88,7 +88,7 @@ "\n", "NCL's `daylight_fao56` calculates the maximum number of daylight hours as described in the Food and Agriculture Organization (FAO) Irrigation and Drainage Paper 56 [(Chapter 3, Equation 34)](https://www.fao.org/4/X0490E/x0490e07.htm#chapter%203%20%20%20meteorological%20data) {footcite}`allan_fao_1998`.\n", "\n", - "Where the maximum number of daylight hours, {math}`N`:\n", + "Where the maximum number of daylight hours, {math}`N`, is:\n", "\n", "{math}`N = \\frac{24}{{\\pi}} {\\omega}_{s}`\n", "\n",