easyclimate.field.monsoon.index_npwi¶
Objective globally unified summer monsoon onset or retreat dates
Functions¶
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Calculate the normalized precipitable water index (NPWI). |
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The refined monsoon regions. |
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Calculate the summer monsoon onset date. |
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Calculate the summer monsoon retreat date. |
Module Contents¶
- easyclimate.field.monsoon.index_npwi.calc_index_NPWI(precipitable_water_daily_data: xarray.DataArray, time_dim: str = 'time') xarray.DataArray¶
Calculate the normalized precipitable water index (NPWI).
\[\mathrm{NPWI} = \frac{\mathrm{PW} - \mathrm{PW_{min}}}{\mathrm{PW_{max}} - \mathrm{PW_{min}}}\]Parameters¶
- precipitable_water_daily_data:
xarray.DataArray. Daily precipitable water data.
- time_dim:
str. The time coordinate dimension name.
Returns¶
Normalized precipitable water index (NPWI).
Reference¶
Zeng, X., and E. Lu, 2004: Globally Unified Monsoon Onset and Retreat Indexes. J. Climate, 17, 2241–2248, https://journals.ametsoc.org/view/journals/clim/17/11/1520-0442_2004_017_2241_gumoar_2.0.co_2.xml.
Tang Xu, Chen Baode, Liang Ping, Qian Weihong. Definition and features of the north edge of Asian summer monsoon. Acta Meteorologica Sinica (Chinese), 2009, (1): 83-89. doi: http://dx.doi.org/10.11676/qxxb2009.009
- precipitable_water_daily_data:
- easyclimate.field.monsoon.index_npwi.find_PW_monsoon_region(precipitable_water_daily_data: xarray.DataArray, time_dim: str = 'time') xarray.DataArray¶
The refined monsoon regions.
Note
To refine the definition of monsoon regions on a grid- cell-by-cell basis, we first compute the 10-yr-averaged monthly PW over each cell. Then we obtain the maximum monthly PW during the three summer months [e.g., June–August in the Northern Hemisphere (NH), denoted as PWw], and the maximum monthly PW during the three winter months (e.g., December–February for the NH, denoted as PWc). The refined monsoon regions are simply defined as grid cells that are within the monsoon regions given in the above studies and have a difference between PWw and PWc greater than 12 mm. Initially we have also tried to use the annual maximum and minimum monthly PW values.
Parameters¶
- precipitable_water_daily_data:
xarray.DataArray. Daily precipitable water data.
- time_dim:
str. The time coordinate dimension name.
Reference¶
Zeng, X., and E. Lu, 2004: Globally Unified Monsoon Onset and Retreat Indexes. J. Climate, 17, 2241–2248, https://journals.ametsoc.org/view/journals/clim/17/11/1520-0442_2004_017_2241_gumoar_2.0.co_2.xml.
Tang Xu, Chen Baode, Liang Ping, Qian Weihong. Definition and features of the north edge of Asian summer monsoon. Acta Meteorologica Sinica (Chinese), 2009, (1): 83-89. doi: http://dx.doi.org/10.11676/qxxb2009.009
Example(s) related to the function¶
- precipitable_water_daily_data:
- easyclimate.field.monsoon.index_npwi.calc_NPWI_monsoon_onset(NPWI: xarray.DataArray, thresh: float = 0.618, consecutive_days: int = 3, n: int = 7, lon_dim: str = 'lon', lat_dim: str = 'lat', time_dim: str = 'time') xarray.DataArray¶
Calculate the summer monsoon onset date.
The summer monsoon onset date for grid cell G is defined as the first day (\(d\)) when NWPI is greater than the Golden Ratio (0.618) for three consecutive days in seven of the nine cells centered at cell G in day \(d\) or (\(d \pm 1\)).
Note
If one or more of the nine grids are undefined, for example, at the edge of monsoon regions, the required number of seven is correspondingly reduced. For instance, if only seven grid cells are defined, the required number is five.
Parameters¶
- NPWI:
xarray.DataArray. Normalized precipitable water index (NPWI).
Attention
It must include three dimensions: time, longitude, and latitude.
- thresh:
float, default: 0.618. Golden Ratio value for the threshold value.
- consecutive_days:
int, default: 3. Consecutive days values.
- n:
int, default: 7. \(n\) of the nine cells centered at cell G in day \(d\) or (\(d \pm 1\)).
- lat_dim:
str, default: lat. Latitude coordinate dimension name. By default extracting is applied over the lat dimension.
- lon_dim:
str, default: lon. Longitude coordinate dimension name. By default extracting is applied over the lon dimension.
- time_dim:
str, default: time. The time coordinate dimension name.
Returns¶
Summer monsoon onset date.
Reference¶
Zeng, X., and E. Lu, 2004: Globally Unified Monsoon Onset and Retreat Indexes. J. Climate, 17, 2241–2248, https://journals.ametsoc.org/view/journals/clim/17/11/1520-0442_2004_017_2241_gumoar_2.0.co_2.xml.
Tang Xu, Chen Baode, Liang Ping, Qian Weihong. Definition and features of the north edge of Asian summer monsoon. Acta Meteorologica Sinica (Chinese), 2009, (1): 83-89. doi: http://dx.doi.org/10.11676/qxxb2009.009
Example(s) related to the function¶
- NPWI:
- easyclimate.field.monsoon.index_npwi.calc_NPWI_monsoon_retreat(NPWI: xarray.DataArray, monsoon_onset_date: xarray.DataArray, thresh: float = 0.618, consecutive_days: int = 3, n: int = 7, lon_dim: str = 'lon', lat_dim: str = 'lat', time_dim: str = 'time') xarray.DataArray¶
Calculate the summer monsoon retreat date.
The summer monsoon retreat date for grid cell G is defined as the first day (\(d\)) when NWPI is less than the Golden Ratio (0.618) for three consecutive days in seven of the nine cells centered at cell G in day \(d\) or (\(d \pm 1\)).
Note
If one or more of the nine grids are undefined, for example, at the edge of monsoon regions, the required number of seven is correspondingly reduced. For instance, if only seven grid cells are defined, the required number is five.
Parameters¶
- NPWI:
xarray.DataArray. Normalized precipitable water index (NPWI).
Attention
It must include three dimensions: time, longitude, and latitude.
- monsoon_onset_date:
xarray.DataArray. Summer monsoon onset date. The results is generated by
easyclimate.index.calc_NPWI_monsoon_onset.- thresh:
float, default: 0.618. Golden Ratio value for the threshold value.
- consecutive_days:
int, default: 3. Consecutive days values.
- n:
int, default: 7. \(n\) of the nine cells centered at cell G in day \(d\) or (\(d \pm 1\)).
- lat_dim:
str, default: lat. Latitude coordinate dimension name. By default extracting is applied over the lat dimension.
- lon_dim:
str, default: lon. Longitude coordinate dimension name. By default extracting is applied over the lon dimension.
- time_dim:
str, default: time. The time coordinate dimension name.
Returns¶
Summer monsoon retreat date.
Reference¶
Zeng, X., and E. Lu, 2004: Globally Unified Monsoon Onset and Retreat Indexes. J. Climate, 17, 2241–2248, https://journals.ametsoc.org/view/journals/clim/17/11/1520-0442_2004_017_2241_gumoar_2.0.co_2.xml.
Tang Xu, Chen Baode, Liang Ping, Qian Weihong. Definition and features of the north edge of Asian summer monsoon. Acta Meteorologica Sinica (Chinese), 2009, (1): 83-89. doi: http://dx.doi.org/10.11676/qxxb2009.009
Example(s) related to the function¶
- NPWI: