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7 | 7 | "source": [ |
8 | 8 | "# Sea Ice\n", |
9 | 9 | "\n", |
10 | | - "The sea ice component of CESM is CICE. This is developed by the [CICE Consortium](https://github.com/CICE-Consortium/CICE). Note that CESM2 uses CICE version 5. In version 6 of CICE, the vertical thermodynamics was separated into a submodule known as Icepack. CICE6 will be the sea ice component in CESM3. \n", |
| 10 | + "The sea ice component of CESM is CICE. This is developed by the [CICE Consortium](https://github.com/CICE-Consortium/CICE). Note that CESM3 uses CICE version 6. In version 6 of CICE, the vertical thermodynamics was separated into a submodule known as Icepack.\n", |
11 | 11 | "\n", |
12 | 12 | "It can be useful for people interested in sea ice science to run simulations with only active sea ice and ocean components and atmospheric forcing. In this exercise, you will learn how to run one of these ice-ocean simulations.\n", |
13 | 13 | "\n", |
|
46 | 46 | "metadata": {}, |
47 | 47 | "source": [ |
48 | 48 | "- This exercise uses the same code base as the rest of the tutorial. \n", |
49 | | - "- You will be using the G compset at the T62_g37 resolution.\n", |
| 49 | + "- You will be using the G compset at the TL319_tx2_3v3 resolution.\n", |
50 | 50 | "- You will run a control simulation and two experimental simulations. Each simulation will be run for one year. \n", |
51 | 51 | "- You will use simple, command line netcdf tools to evaluate how the experiments differ from the control simulation." |
52 | 52 | ] |
|
66 | 66 | "source": [ |
67 | 67 | "<div class=\"alert alert-info\" style=\"text-align: center;\">\n", |
68 | 68 | "\n", |
69 | | - "[CESM CICE User's Guide](https://www.cesm.ucar.edu/models/cesm2/sea-ice)\n", |
| 69 | + "[CESM CICE User's Guide](https://cesm-cice.readthedocs.io/en/latest/)\n", |
70 | 70 | "\n", |
71 | 71 | "</div>" |
72 | 72 | ] |
|
106 | 106 | "id": "68ca54e2-d8ad-41bc-be8f-31a85eec6e65", |
107 | 107 | "metadata": {}, |
108 | 108 | "source": [ |
109 | | - "\n", |
| 109 | + "<div class=\"alert alert-info\" style=\"text-align: center;\">\n", |
| 110 | + " \n", |
| 111 | + "2000_DATM%JRA-1p5-2023_SLND_CICE_MOM6_DROF%JRA-1p5-2023_SGLC_WW3_SESP\n", |
110 | 112 | "\n", |
111 | | - "*<p style=\"text-align: center;\"> Figure: G Compset definition. </p>*" |
| 113 | + "</div>" |
112 | 114 | ] |
113 | 115 | }, |
114 | 116 | { |
|
118 | 120 | "source": [ |
119 | 121 | "<div class=\"alert alert-info\" style=\"text-align: center;\">\n", |
120 | 122 | "\n", |
121 | | - "[Compset Definitions](https://www2.cesm.ucar.edu/models/cesm2/config/compsets.html)\n", |
| 123 | + "[Compset Definitions]()\n", |
122 | 124 | "\n", |
123 | 125 | "</div>" |
124 | 126 | ] |
|
137 | 139 | "metadata": {}, |
138 | 140 | "source": [ |
139 | 141 | "There are two types of temporal forcing for G compsets:\n", |
140 | | - "- Normal Year Forcing (NYF) is 12 months of atmospheric data (like a climatology) that repeats every year. NYF is the default forcing.\n", |
141 | | - "- Interannual varying forcing (GIAF) is forcing that varies by year over the time period (1948-2017). \n", |
| 142 | + "- Repeated Year Forcing (RYF) is 12 months of atmospheric data (like a climatology) that repeats every year.\n", |
| 143 | + "- Interannual varying forcing (G_IAF) is forcing that varies by year over the time period (1958-2023). \n", |
142 | 144 | "\n", |
143 | 145 | "There are two datasets that can be used for G compsets:\n", |
144 | 146 | "- JRA55-do atmospheric data \\([Tsujino et al. 2018](https://doi.org/10.1016/j.ocemod.2018.07.002)\\)\n", |
145 | | - "- Coordinated Ocean-ice Reference Experiments (CORE) version 2 atmospheric data \\([Large and Yeager 2009](http://doi.org/10.1007/s00382-008-0441-3)\\).\n", |
| 147 | + "- Coordinated Ocean-ice Reference Experiments (CORE) version 2 atmospheric data \\([Large and Yeager 2009](http://doi.org/10.1007/s00382-008-0441-3)\\). Note that CORE is being phased out with CESM3.\n", |
146 | 148 | "\n", |
147 | | - "In these exercises we will use the CORE NYF." |
| 149 | + "In these exercises we will use the JRA55 RYF." |
148 | 150 | ] |
149 | 151 | }, |
150 | 152 | { |
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