Extended the description of quantile mapping with text and images

README.md

@@ -20,7 +20,7 @@
 
 This Python module serves as a collection of different scale- and distribution-based bias correction techniques for climatic research
 
-The documentation is available at: [https://python-kraken-sdk.readthedocs.io/en/stable/](https://python-kraken-sdk.readthedocs.io/en/stable/)
+The documentation is available at: [https://python-cmethods.readthedocs.io/en/stable/](https://python-cmethods.readthedocs.io/en/stable/)
 
 > ⚠️ For the application of bias corrections on _lage data sets_ it is recomanded to use the command-line tool [BiasAdjustCXX](https://github.com/btschwertfeger/BiasAdjustCXX) since bias corrections are complex statistical transformation which are very slow in Python compared to the C++ implementation.
 
@@ -78,6 +78,17 @@ All methods except the `adjust_3d` function requires that the input data sets on
 | `quantile_delta_mapping` | Quantile Delta Mapping (additive and multiplicative)                                                                                                         |
 | `adjust_3d`              | requires a method name and the respective parameters to adjust all time series of a 3-dimensional data set                                                   |
 
+Except for the variance scaling, all methods can be applied on stochastic and non-stochastic
+climate variables. Variance scaling can only be applied on non-stochastic climate variables.
+
+- Stochastic climate variables are those that are subject to random fluctuations
+  and are not predictable. They have no predictable trend or pattern. Examples of
+  stochastic climate variables include precipitation, air temperature, and humidity.
+
+- Non-stochastic climate variables, on the other hand, have clear trend and pattern histories
+  and can be readily predicted. They are often referred to as climate elements and include
+  variables such as water temperature and air pressure.
+
 ---
 
 <a name="installation"></a>
@@ -119,7 +130,7 @@ qdm_result = cm.adjust_3d( # 3d = 2 spatial and 1 time dimension
 )
 # to calculate the relative rather than the absolute change,
 # '*' can be used instead of '+' (this is prefered when adjusting
-# ratio based variables like precipitation)
+# stochastic variables like precipitation)
 ```
 
 Notes:

cmethods/__init__.py

@@ -60,8 +60,16 @@ class CMethods:
             * Quantile Mapping :func:`cmethods.CMethods.quantile_mapping`
             * Quantile Delta Mapping :func:`cmethods.CMethods.quantile_delta_mapping`
 
-    Except for the Variance Scaling all methods can be applied on both, interval- and ratio- based
-    variables. The Variance Scaling can only be applied on interval-based variables.
+    Except for the Variance Scaling all methods can be applied on both, stochastic and non-stochastic
+    variables. The Variance Scaling can only be applied on stochastic climate variables.
+
+    Stochastic climate variables are those that are subject to random fluctuations
+    and are not predictable. They have no predictable trend or pattern. Examples of
+    stochastic climate variables include precipitation, air temperature, and humidity.
+
+    Non-stochastic climate variables, on the other hand, have clear trend and pattern histories
+    and can be readily predicted. They are often referred to as climate elements and include
+    variables such as water temperature and air pressure.
     """
 
     SCALING_METHODS = ["linear_scaling", "variance_scaling", "delta_method"]
@@ -362,8 +370,8 @@ def linear_scaling(
         **kwargs,
     ) -> np.array:
         r"""
-        The Linear Scaling bias correction technique can be applied on interval- and
-        ratio-based climate variables to minimize deviations in the mean values
+        The Linear Scaling bias correction technique can be applied on stochastic and
+        non-stochastic climate variables to minimize deviations in the mean values
         between predicted and observed time-series of past and future time periods.
 
         Since the multiplicative scaling can result in very high scaling factors,
@@ -412,8 +420,8 @@ def linear_scaling(
         :type simp: xr.core.dataarray.DataArray
         :param group: The grouping defines the basis of the mean, defaults to ``time.month``
         :type group: Union[str, None], optional
-        :param kind: The kind of the correction, additive for interval- and multiplicative
-            for ratio-based variables, defaults to ``+``
+        :param kind: The kind of the correction, additive for non-stochastic and multiplicative
+            for stochastic climate variables, defaults to ``+``
         :type kind: str, optional
         :raises NotImplementedError: If the kind is not in (``+``, ``*``, ``add``, ``mult``)
         :return: The bias-corrected time series
@@ -474,7 +482,7 @@ def variance_scaling(
         **kwargs,
     ) -> np.array:
         r"""
-        The Variance Scaling bias correction technique can be applied on interval-based
+        The Variance Scaling bias correction technique can be applied only on non-stochastic
         climate variables to minimize deviations in the mean and variance
         between predicted and observed time-series of past and future time periods.
 
@@ -532,7 +540,7 @@ def variance_scaling(
         :type simp: xr.core.dataarray.DataArray
         :param group: The grouping defines the basis of the mean, defaults to ``time.month``
         :type group: Union[str, None], optional
-        :param kind: The kind of the correction, additive for interval-based variables,
+        :param kind: The kind of the correction, additive for non-stochastic climate variables
             no other kind is available so far, defaults to ``+``
         :type kind: str, optional
         :raises NotImplementedError: If the kind is not in (``+``, ``add``)
@@ -600,8 +608,8 @@ def delta_method(
         **kwargs,
     ) -> np.array:
         r"""
-        The Delta Method bias correction technique can be applied on interval- and
-        ratio-based climate variables to minimize deviations in the mean values
+        The Delta Method bias correction technique can be applied on stochastic and
+        non-stochastic climate variables to minimize deviations in the mean values
         between predicted and observed time-series of past and future time periods.
 
         Since the multiplicative scaling can result in very high scaling factors,
@@ -651,8 +659,8 @@ def delta_method(
         :type simp: xr.core.dataarray.DataArray
         :param group: The grouping defines the basis of the mean, defaults to ``time.month``
         :type group: Union[str, None], optional
-        :param kind: The kind of the correction, additive for interval- and multiplicative
-            for ratio-based variables, defaults to ``+``
+        :param kind: The kind of the correction, additive for non-stochastic and multiplicative
+            for stochastic climate variables, defaults to ``+``
         :type kind: str, optional
         :raises NotImplementedError: If the kind is not in (``+``, ``*``, ``add``, ``mult``)
         :return: The bias-corrected time series
@@ -734,14 +742,39 @@ def quantile_mapping(
         After the Quantile Mapping was applied, the mean is shifted back. Since it does not make sens
         to take the whole mean to rescale the data, the month-dependent long-term mean is used.
 
-        In the following the equations of Alex J. Cannon (2015) are shown (without detrending):
+        In the following the equations of Alex J. Cannon (2015) are shown and explained (without detrending):
 
         **Additive**:
 
             .. math::
 
                 X^{*QM}_{sim,p}(i) = F^{-1}_{obs,h} \left\{F_{sim,h}\left[X_{sim,p}(i)\right]\right\}
 
+
+            The additive quantile mapping procedure consists of inserting the value to be
+            adjusted (:math:`X_{sim,p}(i)`) into the cumulative distribution function
+            of the modeled data of the control period (:math:`F_{sim,h}`). This determines,
+            in which quantile the value to be adjusted can be found in the modeled data of the control period
+            The following images show this by using :math:`T` for temperatures.
+
+            .. figure:: ../_static/images/qm-cdf-plot-1.png
+                :width: 600
+                :align: center
+                :alt: Determination of the quantile value
+
+                Fig 1: Inserting :math:`X_{sim,p}(i)` into :math:`F_{sim,h}` to determine the quantile value
+
+            This value, which of course lies between 0 and 1, is subsequently inserted
+            into the inverse cumulative distribution function of the reference data of the control period to
+            determine the bias-corrected value at time step :math:`i`.
+
+            .. figure:: ../_static/images/qm-cdf-plot-2.png
+                :width: 600
+                :align: center
+                :alt: Determination of the QM bias-corrected value
+
+                Fig 1: Inserting the quantile value into :math:`F^{-1}_{obs,h}` to determine the bias-corrected value for time step :math:`i`
+
         **Multiplicative**:
 
             .. math::
@@ -759,12 +792,16 @@ def quantile_mapping(
         :type simp: xr.core.dataarray.DataArray
         :param n_quantiles: Number of quantiles to respect/use
         :type n_quantiles: int
-        :param kind: The kind of the correction, additive for interval- and multiplicative
-            for ratio-based variables, defaults to ``+``
+        :param kind: The kind of the correction, additive for non-stochastic and multiplicative
+            for stochastic climate variables, defaults to ``+``
         :type kind: str, optional
         :param detrended: If the extremes should be respected by applying month-dependent
             detrending before and after applying the Quantile Mapping
         :type detrended: bool, optional
+        :param val_min: Lower boundary for interpolation (only if ``kind="*"``, default: ``0``)
+        :type val_min: float, optional
+        :param val_max: Upper boundary for interpolation (only if ``kind="*"``, default: ``None``)
+        :type val_max: float, optional
         :raises NotImplementedError: If the kind is not in (``+``, ``*``, ``add``, ``mult``)
         :return: The bias-corrected time series
         :rtype: np.array
@@ -990,8 +1027,8 @@ def quantile_delta_mapping(
         :type simp: xr.core.dataarray.DataArray
         :param n_quantiles: Number of quantiles to respect/use
         :type n_quantiles: int
-        :param kind: The kind of the correction, additive for interval- and multiplicative
-            for ratio-based variables, defaults to ``+``
+        :param kind: The kind of the correction, additive for non-stochastic and multiplicative
+            for non-stochastic climate variables, defaults to ``+``
         :type kind: str, optional
         :raises NotImplementedError: If the kind is not in (``+``, ``*``, ``add``, ``mult``)
         :return: The bias-corrected time series
@@ -1125,7 +1162,7 @@ def get_inverse_of_cdf(
         xbins: Union[list, np.array],
     ) -> np.array:
         r"""
-        Returns the inverse cumulative distribution function of with the following
+        Returns the inverse cumulative distribution function as:
         :math:`F^{-1}_{x}\left[y\right]` where :math:`x` represents ``base_cdf`` and
         ``insert_cdf`` is represented by :math:`y`.
 
@@ -1152,7 +1189,7 @@ def get_adjusted_scaling_factor(
 
             where:
                 - :math:`x` is ``factor``
-                - :math:`y` is ``max_scaling_factor``.
+                - :math:`y` is ``max_scaling_factor``
 
         :param factor: The value to check for
         :type factor: Union[int, float]

docs/src/introduction.rst

@@ -16,7 +16,7 @@ time periods. Data from past periods are used to adjust variables
 from current and future time series so that their distributional
 properties approximate possible actual values.
 
-.. figure:: ../images/biasCdiagram.png
+.. figure:: ../_static/images/biasCdiagram.png
     :width: 600
     :align: center
     :alt: Schematic representation of a bias adjustment procedure
@@ -31,7 +31,7 @@ It is directly visible that the delta adjusted time series
 (:math:`T^{*DM}_{sim,p}`) are much more similar to the observed data (:math:`T_{obs,p}`)
 than the raw modeled data (:math:`T_{sim,p}`).
 
-.. figure:: ../images/dm-doy-plot.png
+.. figure:: ../_static/images/dm-doy-plot.png
     :width: 600
     :align: center
     :alt: Temperature per day of year in modeled, observed and bias-adjusted climate data
@@ -56,6 +56,17 @@ All of these methods are intended to be applied on 1-dimensional time-series cli
 This module also provides the function :func:`cmethods.CMethods.adjust_3d` that enables
 the application of the desired bias correction method on 3-dimensinoal data sets.
 
+Except for the variance scaling, all methods can be applied on stochastic and non-stochastic
+climate variables. Variance scaling can only be applied on non-stochastic climate variables.
+
+- Stochastic climate variables are those that are subject to random fluctuations
+  and are not predictable. They have no predictable trend or pattern. Examples of
+  stochastic climate variables include precipitation, air temperature, and humidity.
+
+- Non-stochastic climate variables, on the other hand, have clear trend and pattern histories
+  and can be readily predicted. They are often referred to as climate elements and include
+  variables such as water temperature and air pressure.
+
 Examples can be found in the `python-cmethods`_ repository and of course
 within this documentation.