Meterological Lake Comparison
  • Home
  • Overview
  • Methods
  • Time Series
  • Metrics & stats
  • Seasonal and event behaviour
  • Rotorua demo
  • Reproducibility
  • References

Table of Content

  • Objective
  • Data sources
  • Outputs

Meterological Source Comparison

Overview

Meteorological data is utilised for many different lake assessments, from understanding lake regime shifts to modelling future lake dynamics (Freshwater Ecology : Concepts and Environmental Applications of Limnology 2020). It is therefore vital to use the best available meteorological data for the location and time of choice. Too often meteorological data are incomplete and unreliable. ERA5 (ECMWF fifth gen) data gridded at 9km (Setchell, n.d.) is widely used due to its comprehensive and clean nature, combining observations with model data, however, it is more coarse than other available sources and some variables are known to misrepresent data at the lake surface (low atmosphere meteorology). NIWAs virtual climate station network takes captured observational station data and creates a 5km grid connecting other weather stations and integrates data in a chosen location. The VCSN data is somewhat intertwined with the Airport data, which is used as the Reference for the Rotorua Lake demo. Meteorological datasets in more densely populated areas or with large topographical gradients will typically result in micro-climatic datasets due to the physical nature of these environments. In partucular wind, rain and even temperature in larger cities. Additionally, stations placed in higher altitudes can often misrepresent lower altitudes. When using datasets for lake specific projects Buoy data has the opportunity to allow for more accurate readings due to its on water position. However, precipitation data is often inaccurate, especially in higher wind events, causing movement of monitoring equipment. This is especially true in large lakes that can develop substantial waves. For this reason, wind can also be skewed in events. Temperature for a given lake from a Buoy is regarded the most likely accurate candidate, as fluctuations from a water body and fluxes from land follow different physical laws.

The question here is how coarse global, modelled national, Local observational, and Lake source meteorological data compare. Is there a better data source in cool or warm periods? how about in a storm event? or for a specific variable? and perhapse there a better data source for local models?

Objective

To analyse different meteorological data available for a given location, access accuracy, precision, bias and overall agreement.

Data sources

Limnotrack Buoy on lake, NIWA virtual climate station network (VCSN), ERA5 statlite data, Observational data “Airport” station, Observational data “Town” station.

Data source and station names will vary from location to location. Selecting stations from these websites is laid out in the reproducibility tab, methods tab and 02_prepare_raw_data R script.

Outputs

The outputs of this project will show:

  1. Correlation coefficient (Pearsons r)

  2. Change in intercept and slope (linear regression slope and intercept)

  3. Mean absolute error (MAE)

  4. Root mean squared error (RMSE)

  5. Concordance correlation coefficient (CCC)

  6. Mean and relative bias (%)

  7. Event score

  8. Rolling window/drift

  9. Probability detection (POD)

  10. False alarm ratio (FAR)

  11. Critical success index (CSI)

    These metrics along with plots and diagnostics, will answer bias questions, seasonal behaviour, event disagreement and extremes

References

Freshwater Ecology : Concepts and Environmental Applications of Limnology. 2020. 3rd edition. Aquatic Ecology. San Diego, Calif.: Academic Press.
Setchell, Helen. n.d. “ECMWF Reanalysis V5.”