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TEAM 12: Agro-Climatic zones - Europa

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Page 1: TEAM 12: Agro-Climatic zones - Europa

TEAM 12: Agro-Climatic zones

1

Page 2: TEAM 12: Agro-Climatic zones - Europa

Delimiting of Agro-Climatic zones

• Karel Jedlička, Pavel Hájek, Karl Gutbrodt, Marcela Doubková, ApurvaKochar

• www.euxdat.eu

INSPIRE Conference, Antwerp, 19th Sept 2018

Page 3: TEAM 12: Agro-Climatic zones - Europa

(EUXDAT agriculture e-infrastructure)

• Emerging cloud platform

• Client side: web based coding environment• Jupyter notebooks & Python

• Server side (HPC):• GDAL/OGR

• Sen2Agri

• (GRASS)

• …

INSPIRE Conference, Antwerp, 19th Sept 2018

Page 4: TEAM 12: Agro-Climatic zones - Europa

Delimiting of Agro-Climatic Zones

• Goal: to provide local agro-climatic maps by processing detailed EO data and climate model data.

• Data:• General weather conditions (large-scale weather models ~ Meteoblue API)• Local topography (elevation, North/South slopes ~ EU-DEM)• Hydrology ~ buffer effects, such as rivers, lakes, sea or swamps (OpenStreetMap)• Soil types (OLU).

• Initial experiments: • Elevation as a factor influencing temperature• Slope orientation as a factor influencing temperature• Hydrology as a factor influencing temperature• …

• Verification: meteorological expert needed

INSPIRE Conference, Antwerp, 19th Sept 2018

Page 5: TEAM 12: Agro-Climatic zones - Europa

Delimiting of Agro-Climatic Zones

• Elevation as a factor influencing temperature• Temperature on Earth’s surface decreases averagely by 0.65 °C for each 100

meters of elevation (under normal weather circumstances)

• Temperatures provided by global meteorological models are related a lattice of particular geographic positions (with elevation defined as an elevation 2 m above Earth’s surface)

• DEMs used by global meteo modelsare sparse

INSPIRE Conference, Antwerp, 19th Sept 2018

Page 6: TEAM 12: Agro-Climatic zones - Europa

Delimiting of Agro-Climatic Zones

• Elevation as a factor influencing temperature• Input ~ sparse DEM (with approx. 4x4 km sampling)

of temperatures estimated on earth‘s surfacereduction to sea level:

T0 = Ts + k * Es /100

• Densification of the 4x4 km DEM T0 temperature to 25 x 25 m spacing DEM using spline interpolation.

• Applying the elevation factor to calculate temperatures back on surface, but on DEM with25x25 m spacing.

Ts = T0 - k * Es /100

INSPIRE Conference, Antwerp, 19th Sept 2018

Page 7: TEAM 12: Agro-Climatic zones - Europa

Delimiting of Agro-Climatic Zones

• Elevation as a factor influencing temperature• Temperatures on Surface (sparse)

• Temperatures reduction to sea level

• Applying the elevation factor back

Page 8: TEAM 12: Agro-Climatic zones - Europa

Delimiting of Agro-Climatic Zones

• Elevation as a factor influencing temperature

before after

Page 9: TEAM 12: Agro-Climatic zones - Europa

Delimiting of Agro-Climatic Zones

• Hydrology as a factor influencing temperature• Water accumulates thermal

energy from sun and neighborhood.

• Water has much longer thermal inertia than air.

• Water smooths the daily temperature changes (lowering the temperature during the hot period of a day and increasing the temperature during night).

• Such an influence subsides with a distance from the water reservoir.

• Talking technically

• Water reservoirs keep an average day temperature.

• Water influence to temperaturedecreases inversely in proportion to distance (the closer a place is to the water, the more influence)

• The influence ends in 1 km distance.

INSPIRE Conference, Antwerp, 19th Sept 2018

Page 10: TEAM 12: Agro-Climatic zones - Europa

Delimiting of Agro-Climatic Zones

• Hydrology as a factor influencing temperature• Clean hydrologic data to exclude irrelevant water reservoirs

• Calculation of the hydrologic effect to the temperature of a selected day hour

INSPIRE Conference, Antwerp, 19th Sept 2018

Page 11: TEAM 12: Agro-Climatic zones - Europa

Delimiting of Agro-Climatic Zones

• Hydrology as a factor influencing temperature• Clean hydrologic data to exclude irrelevant water reservoirs

• Water areas ~ exclude areas smaller than a treshold

• Water streams ~ exclude upper streams shorten than a treshold

• Apply Strahler ordering

• Exclude streams of 1st order shorter than a treshold 1

1

11 1

2

2 2

3INSPIRE Conference, Antwerp, 19th Sept 2018

Page 12: TEAM 12: Agro-Climatic zones - Europa

Delimiting of Agro-Climatic Zones

• Hydrology as a factor influencing temperature• Calculation of the hydrologic effect to temperature at noon

Temperature on the surface at noon

Average day temperature on the surface

Transition zone effect

26 25 25 25 25 25 25 25 25 26 26

21 20 20 20 20 20 20 20 20 20 21

25 25 25 25 25 25 25 25 26 26 26

26 26 25 25 25 25 25 25 25 25 25

1 1 0.8 0.5 0.2 0 0.2 0.5 0.8 1 1

26 25 24 22.5 21 20 20 21 22.5 26 26Temperature on the surface at noonwith hydro effect

Ts-hour-hydro = Ts-mean + (Ts-hour - Ts-mean) * (Zinfluence)Ts-hour-hydro

Ts-mean

Ts-hour

Zinfluence

Page 13: TEAM 12: Agro-Climatic zones - Europa

Delimiting of Agro-Climatic Zones

• Hydrology as a factor influencing temperature• Calculation of the hydrologic effect to 12 a.m. temperature

T> 0°C

Ts-noon-hydroTs-mean Ts-noon

T< 0°C

Page 14: TEAM 12: Agro-Climatic zones - Europa

Delimiting of Agro-Climatic Zones

• Hydrology as a factor influencing temperature• Calculation of the hydrologic effect to 6 a.m. temperature

(because freezing areas are of interest for agriculture)

T< 0°C

T> 0°C

Ts-dawn-hydroTs-mean Ts-dawn

Page 15: TEAM 12: Agro-Climatic zones - Europa

Delimiting of Agro-Climatic Zones

• Status of the art• Initial experiments performed• Verification: meteorological expert needed

INSPIRE Conference, Antwerp, 19th Sept 2018

Ts-dawn(25x15m)-hydroTs-dawn (4x4 km) Ts-dawn (25x25m)

Page 16: TEAM 12: Agro-Climatic zones - Europa

HACKATHON RELATED QUESTIONS

• …

INSPIRE Conference, Antwerp, 19th Sept 2018

Page 17: TEAM 12: Agro-Climatic zones - Europa

DATA

• Input data• EU-DEM – digital surface model (DSM) of EEA member and cooperating

countries representing the first surface as illuminated by the sensors. Ahybrid product based on SRTM and ASTER GDEM data fused by a weighted averaging approach.License: Copernicus data and information policy Regulation (EU) No 1159/2013

• Meteoblue weather API – commercial purchase (free for EUXDAT Project

• Output data – not yet produced. Will be a part of the EUXDAT agriculture e-infrastructure

INSPIRE Conference, Antwerp, 19th Sept 2018

Page 18: TEAM 12: Agro-Climatic zones - Europa

SOFTWARE & TOOLS

• Proof of concept to be used in the EUXDAT agriculture e-infrastructure

INSPIRE Conference, Antwerp, 19th Sept 2018

Page 19: TEAM 12: Agro-Climatic zones - Europa

USE OF APIs

• Meteoblue weather API

INSPIRE Conference, Antwerp, 19th Sept 2018

Page 20: TEAM 12: Agro-Climatic zones - Europa

COPERNICUS RELEVANCE

• Using Copernicus data (EU-DEM)

INSPIRE Conference, Antwerp, 19th Sept 2018

Page 21: TEAM 12: Agro-Climatic zones - Europa

INTEROPERABILITY

• the EUXDAT agriculture e-infrastructure is going to serve web basedtools for agriculture advisors by ofering both API and GUI

INSPIRE Conference, Antwerp, 19th Sept 2018

Page 22: TEAM 12: Agro-Climatic zones - Europa

BUSINESS/INNOVATION

• Too early to commercionalize, depends on EUXDAT project

INSPIRE Conference, Antwerp, 19th Sept 2018

Page 23: TEAM 12: Agro-Climatic zones - Europa

CHALLENGES

• Sustainable food production• protecting natural resources and at the same time providing food for the

society

• Efficient agriculture (precision farming)• saving costs, optimising yield and other resources

(e.g. fertilisers)

INSPIRE Conference, Antwerp, 19th Sept 2018

Page 24: TEAM 12: Agro-Climatic zones - Europa

FOLLOW-UP

• Are you ready to continue with follow up actions?• Yes

• Would you like to join effort with other teams from the INSPIRE Hack 2019 to build more advanced solution?• Yes

INSPIRE Conference, Antwerp, 19th Sept 2018

Page 25: TEAM 12: Agro-Climatic zones - Europa

Delimiting of Agro-Climatic Zones

•Questions?

INSPIRE Conference, Antwerp, 19th Sept 2018

Ts-dawn(25x15m)-hydroTs-dawn (4x4 km) Ts-dawn (25x25m)


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