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# HAN_Marine_element | ||
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- 2023年6月18日已全部完成 | ||
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汉の2023春OUC海洋要素计算作业库 | ||
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- 此仓库为中国海洋大学课程:海洋要素计算*(选课号:[070103101251])*的作业而建立 | ||
- 此仓库为中国海洋大学课程:海洋要素计算(选课号:[*070103101251*])的作业而建立 | ||
- 所有者:Hanxue Yu 余汉学 | ||
- 指导教师:王颖颖&杨俊超 | ||
- 参考: | ||
- Github上可以找到的学长多年前写的[代码仓库][先輩のRepo] | ||
- 海洋要素数据的质量控制中的格林布斯准则参考:[c-bata/outlier-utils][glbs] | ||
- WORK2中的EOF计算来自于[Python EOF module][eofs] | ||
- WORK2中的PDO index来自于[PDO index][pdo] | ||
- WORK4中计算比容异常[GSW-Python][gsw] | ||
- WORK5中cmap "Rocket"来自于[seaborn: statistical data visualization][seaborn] | ||
- 刘永玲.杜凌.李静凯.翟方国 海洋要素计算上机实验指导书[M] 青岛:中国海洋大学出版社,2021 | ||
- GB/T 14914.6-2021, 海洋观测规范 第6部分:数据处理与质量控制[S]. | ||
- [GSW-Python][gsw] | ||
- 字体[LXGW Bright][lxgw] | ||
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## 作业一 [海洋要素数据的质量控制][def1] | ||
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- 1.**奇异值判定与处理,生成新序列** | ||
- 2.**分析两序列的平均值、标准差等统计特征的变化** | ||
- 拓展作业见[拓展作业-空间二位插值][def1_d] | ||
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![WORK1代表图片](WORK1\results.png) | ||
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## 作业二 [利用EOF方法研究北太平洋海表面温度总体时空变化特征][def2] | ||
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- 选取1900-2020年为研究时间段,利用EOF方法对北太平洋海表面温度场数据进行分析。 | ||
- 讨论北太平洋SST在1900-2020年总体时空变化特征 | ||
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![WORK2代表图片](WORK2\results.png) | ||
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## 作业三 [长期水位资料的调和分析][def3] | ||
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<table border=\"1\" class=\"dataframe\"> | ||
<thead> | ||
<tr style=\"text-align: right;\"> | ||
<th></th> | ||
<th>a</th> | ||
<th>b</th> | ||
<th>R</th> | ||
<th>θ</th> | ||
<th>H</th> | ||
<th>g</th> | ||
</tr> | ||
<tr> | ||
<th>分潮</th> | ||
<th></th> | ||
<th></th> | ||
<th></th> | ||
<th></th> | ||
<th></th> | ||
<th></th> | ||
</tr> | ||
</thead> | ||
<tbody> | ||
<tr> | ||
<th>M2</th> | ||
<td>-1460.102843</td> | ||
<td>1239.338306</td> | ||
<td>1915.165724</td> | ||
<td>82.648415</td> | ||
<td>1845.483605</td> | ||
<td>8.659484</td> | ||
</tr> | ||
<tr> | ||
<th>O1</th> | ||
<td>-53.780013</td> | ||
<td>-216.599202</td> | ||
<td>223.175949</td> | ||
<td>-59.769138</td> | ||
<td>276.439846</td> | ||
<td>64.557064</td> | ||
</tr> | ||
<tr> | ||
<th>S2</th> | ||
<td>368.429984</td> | ||
<td>-377.902054</td> | ||
<td>527.778946</td> | ||
<td>-63.498182</td> | ||
<td>527.778946</td> | ||
<td>239.201911</td> | ||
</tr> | ||
<tr> | ||
<th>K1</th> | ||
<td>197.306115</td> | ||
<td>228.400426</td> | ||
<td>301.821898</td> | ||
<td>49.177560</td> | ||
<td>341.978206</td> | ||
<td>307.634942</td> | ||
</tr> | ||
<tr> | ||
<th>P1</th> | ||
<td>51.051973</td> | ||
<td>97.105078</td> | ||
<td>109.707339</td> | ||
<td>62.267323</td> | ||
<td>109.707339</td> | ||
<td>293.144287</td> | ||
</tr> | ||
<tr> | ||
<th>N2</th> | ||
<td>-349.550854</td> | ||
<td>64.514394</td> | ||
<td>355.454506</td> | ||
<td>80.799918</td> | ||
<td>342.521514</td> | ||
<td>317.393238</td> | ||
</tr> | ||
<tr> | ||
<th>Q1</th> | ||
<td>13.719769</td> | ||
<td>-43.172999</td> | ||
<td>45.300551</td> | ||
<td>-72.370479</td> | ||
<td>56.112128</td> | ||
<td>10.179002</td> | ||
</tr> | ||
<tr> | ||
<th>K2</th> | ||
<td>-51.515602</td> | ||
<td>102.913995</td> | ||
<td>115.087565</td> | ||
<td>38.694182</td> | ||
<td>153.633137</td> | ||
<td>72.628583</td> | ||
</tr> | ||
<tr> | ||
<th>M4</th> | ||
<td>34.167625</td> | ||
<td>-87.967445</td> | ||
<td>94.370006</td> | ||
<td>-68.773225</td> | ||
<td>87.627747</td> | ||
<td>17.526245</td> | ||
</tr> | ||
<tr> | ||
<th>MS4</th> | ||
<td>-21.067135</td> | ||
<td>53.356617</td> | ||
<td>57.365083</td> | ||
<td>18.557827</td> | ||
<td>53.266638</td> | ||
<td>248.168533</td> | ||
</tr> | ||
</tbody> | ||
</table> | ||
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![WORK3代表图片](WORK3\results.png) | ||
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## 作业四 [地转流计算][def4] | ||
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## 作业五 [海浪资料统计分析-施工ing 06\07\2023][def5] | ||
![WORK4代表图片](WORK4\2018-01%2010%20dbar.png) | ||
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- 1.利用两月的月平均资料计算北太平洋*6°N-35°N*范围内的地转流,选取**1500db**作为参考零面画出*10db*,*100 db*,*250 db*,*500 db*等四个深度层上的流场和流速 | ||
- 2.利用上面计算结果,计算北赤道流水体输运(如130°E,8°N-18°N断面),比较讨论两月结果差异,也可进一步比较不同断面的差异 | ||
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## 作业五 [海浪资料统计分析][def5] | ||
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- 1. 画出波面高度时间序列,利用上跨零点或者下跨零点的方法读取数据资料中的波高、周期等波浪要素,并画图展示。 | ||
- 2. 画出波高的概率密度分布,并计算给出有效波高和有效波周期 | ||
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![WORK5代表图片](WORK5\result.png) | ||
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[先輩のRepo]: https://github.com/FinalTheory/oceanography-numerical-calculations | ||
[glbs]: https://github.com/c-bata/outlier-utils | ||
[gsw]: https://teos-10.github.io/GSW-Python/gsw_flat.html | ||
[eofs]: https://ajdawson.github.io/eofs/latest/api/eofs.standard.html | ||
[pdo]: https://www.ncei.noaa.gov/access/monitoring/pdo/ | ||
[seaborn]: http:https://seaborn.pydata.org/ | ||
[lxgw]: https://github.com/lxgw/LxgwBright | ||
[def1]: https://nbviewer.org/github/Yuhan-xue/HAN_Marine_element/blob/main/WORK1/WORK1.ipynb | ||
[def1_d]: https://nbviewer.org/github/Yuhan-xue/HAN_Marine_element/blob/main/WORK1/%E6%8B%93%E5%B1%95/%E6%8B%93%E5%B1%951.ipynb | ||
[def2]: https://nbviewer.org/github/Yuhan-xue/HAN_Marine_element/blob/main/WORK2/work2.ipynb | ||
[def2]: https://nbviewer.org/github/Yuhan-xue/HAN_Marine_element/blob/main/WORK2/WORK2.ipynb | ||
[def3]: https://nbviewer.org/github/Yuhan-xue/HAN_Marine_element/blob/main/WORK3/WORK3.ipynb | ||
[def4]: https://nbviewer.org/github/Yuhan-xue/HAN_Marine_element/blob/main/WORK4/WORK4.ipynb | ||
[def5]: https://nbviewer.org/github/Yuhan-xue/HAN_Marine_element/blob/main/WORK5/WORK5.ipynb | ||
[def5]: https://nbviewer.org/github/Yuhan-xue/HAN_Marine_element/blob/main/WORK5/WORK5.ipynb |
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