Environmental Change: Cycle in vegetation Flashcards

1
Q

Earth is Constantly Changing

A
  • Natural change
  • Human caused change
  • Change occurs on various scales
  • Time
  • Wildfires burn over days & weeks
  • Climate change occurs over decades & centuries
  • Space
  • Wildfires burn over 0.1 – 10km2
  • Climate change occurs across the globe
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

Monitoring Environmental Change

A

Valuable for a variety of reasons:

  • Minimize impact on environment
  • Ensure compliance with laws
  • Protect human health
  • Predicting into the future
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

Why would satellite data be advantageous for monitoring environmental change from space?

A
  • standerlized data, efficency,
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

Data Requirements

A
  • Data requirements vary with the type of environmental change studied
  • Selecting suitable data is crucial in successfully detecting environmental change
  • At a minimum you need to know the required:
    o** Level of spatial detail**
    o Region of the electromagnetic spectrum
    o Frequency of re-visit
    o Temporal dimension**
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

1. Level of spatial detail

A
  • More detail generally implies less area covered by single image and bigger file size

Examples:

o Moderate resolution (>25m) is suitable to detect amount of forest lost or gained in an area

o Very fine resolution (<1m) is needed to detect changes at single tree leve

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

Level of Spatial Detail: Spatial resolution

A

Coarse scale
* Ice sheets
* MODIS

Moderate scale
* Land cover
* Landsat

** Fine scale**
* Individual trees
* <1m

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

2. Region of the Electromagnetic Spectrum

A
  • Specific regions of the electromagnetic spectrum where the change occurs
  • Satellite sensors have different spectral resolutions

Examples:
o Broad classes, such as dead or live vegetation, can usually be separated using few, wide bands(like visible, NIR)

o More specific classes, such as different rock types require comparison of many, narrow bands

**the more specific we are trying to get (in terms of category) the more spectrum information were are going to need the more bands we are gonna need **

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

Region of the EMS:Spectral Resolution

A
  • Vegetation health
    o Red
    o NIR
  • NDVI
  • Land cover (vegetation, rock,
    soil, water)
    o More bands needed
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

3. Frequency of re-visit

A

How often do you need to see an area to characterize the change?

Examples:
o Logging/cut blocks
▪ 16-day re-visit sufficient
▪ Landsat

o Fire progression
▪ Daily (or finer)

clouds can also get in the way of that

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

4.Temporal Dimension

A

How long do you need to collect data to be able to characterize the change?

Varies with the scope of study:

Examples:
o Changes in climate are slow, require long term information (>10 years)

o Area burned after a fire event is a fast change, require short term information (a week or two)

  • Aerial imagery is available for the last ~100 years, while satellite only for the last ~50 years
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

Three Types of Change from Remote Sensing

A

Cyclical
Abrupt
Gradual

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

Data Requirements

A
  • As we talk about different kinds of change, and specific examples
  • Consider the data requirements necessary to detect those changes
  • What level of spatial detail is required?
  • i.e. spatial resolution
  • What region of the EMS is required?
  • i.e. spectral resolution
  • What frequency of re-visit is required?
  • i.e. temporal resolution
  • What temporal dimension is required?
  • i.e. how long do we need to be collecting data for
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

Cyclical

Season Cycles

A

A few examples:

  • Temperature
  • Day length
  • Snow cover
  • The greening and browning of
    deciduous vegetation
  • Animal migration
  • Animal hibernation
  • Canadians going to Florida each
    winter!
  • Our hobbies
    o Ski in the winter
    o Hike and bike in the summer
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

Cyclical Patterns

A

A pattern that repeats over time

  • We will focus on:
    o Phenology/vegetation cycles
    ▪ Camera traps
    ▪ MODIS
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

Seasonal Cycles of Snow and Vegetation

A
  • As temperature warms in the summer:
    o Snow melts
    o Vegetation greens up
  • As temperatures cool in the fall:
    o Snow returns
    o Vegetation browns
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

Vegetation Cycles

A

Camera time-lapse photography

  • Set up a network of cameras
    o Or just one if you are only interested in one spot
  • Take one picture each day

o Results in daily RGB(red,green,blue visible light) measurements

16
Q

Time-lapse Camera Data

A

Attributes
* Single point data
* Very fine spatial scale
* Very high temporal resolution
* All weather data
* VIS (RGB) data- 3 bands

Applications
* Understanding understory
phenology
* Validating satellite data
* Analyzing fine scale vegetation
phenology
* In space & time

17
Q

How can we make meaningful measurements from a time-lapse of
photos?

A

We can use what we know about spectral signatures!

18
Q

Quick Note About Cameras

A
  • Cameras function like any other remote sensing instrument

They have a defined spatial resolution
-Pixel size

And use 3 bands
* Red
* Green
* Blue

Additive colour system
* Equal peak brightness of RGB = white

19
Q

healthy vegetation/green vegetation -summer

A

green peaks in reflection

blue and red reflects less

20
Q

unhalthy/brown vegetation-winter and fall

A

red reflectence increses

21
Q

We can derive RGB based phenology metrics (camera trap version of NDVI)

A

2GRBi = 2*Green – (Blue + Red)

Brown vegetation = Low 2GRBi
Green vegetation = High 2GRBi

22
Q

Vegetation Cycles

A

Plot 2GRBi for every day of the year

  • From this curve, we can identify key
    phenology events
  • Greenup: When the leaves emerge
  • Maturity: When 2GRBi is maximum
  • Senescence: When leaves change color and die

a important data requirement for vegetation is daily imagery/frequency revision

23
Q

Time-lapse camera give us a detailed look at vegetation for a few select areas

But what if we want to look at vegetation cycles over large regions?

A

then we use MODIS

24
Q

MODIS data for Vegetation Cycle

A

We can use MODIS data for this
o Daily satellite images
o 250-1000m resolution

  • Allows us to observe how
    vegetation changes through the
    year across the entire planet
25
Q

Compare red reflectance to NIR reflectance
through the growing season

A

As plants greenup, notice how the difference between red and NIR increases

the difference between green and brown vegetation becomes stronger/larger when using NIR compared to red light

26
Q

Calculate a measure of greenness from MODIS images through the
year:

A

NDVI = (NIR – Red) / (NIR + Red)

Brown vegetation = Low NDVI
Green vegetation = High NDVI

27
Q
A

Similar to the cameras:

  • We can plot NDVI through the year for each MODIS pixel
  • And identify key phenology events
    o Greenup, maturity, senescence
  • We can calculate the growing season as the

Length of time between greenup and senescence

28
Q

With years of MODIS observations, we can see how vegetation
cycles look from year to year

A

If we monitor this for many years, we could start to see changes in
the growing season as the climate warms

29
Q

Review of Measuring Vegetation Cycles

A

Two approaches covered:

  • Camera time-lapse
    o Can get detailed information on vegetation cycles for a few areas of interest
  • MODIS data
    o Can get broad-scale information for the whole planet
  • In both techniques, we identify changes in the spectral signature of plants
    o Using different spectral bands

▪ RGB for cameras
➢ 2GRBI
▪ Red & NIR for MODIS
➢ NDVI

30
Q

What are the data requirements if I want to measure global
phenological changes due to climate change?

A
  • low level of spatial detail
  • VIS/NIR ideal
  • Daily measurements required
  • Decades of data required at
    minimum

instrument: MODIS

30
Q

What are the data requirements if I want measure phenological
changes in my backyard due to this year’s drought?

A
  • High level of spatial detail
  • VIS/NIR bands
  • daialy mesurments
  • only 1-2 years of data requirement(temporal dimension)

instrument: camera lapse check all the boxes

31
Q

I want to measure global phenological
changes due to climate change

A
  • Low level of spatial detail
  • VIS/NIR ideal
  • Daily measurements required
  • Decades of data required at minimum

instrument : MODIS