## Vertically integrate profiles (vp or vpts) to an integrated profile (vpi)

### Description

Performs a vertical integration of density, reflectivity and migration traffic rate, and a vertical averaging of ground speed and direction weighted by density.

### Usage

integrate_profile(x, alt_min, alt_max, alpha = NA, interval_max = Inf)

## S3 method for class 'vp'
integrate_profile(
x,
alt_min = 0,
alt_max = Inf,
alpha = NA,
interval_max = Inf
)

## S3 method for class 'list'
integrate_profile(
x,
alt_min = 0,
alt_max = Inf,
alpha = NA,
interval_max = Inf
)

## S3 method for class 'vpts'
integrate_profile(
x,
alt_min = 0,
alt_max = Inf,
alpha = NA,
interval_max = Inf
)


### Arguments

 x A vp or vpts object. alt_min Minimum altitude in m. alt_max Maximum altitude in m. alpha Migratory direction in clockwise degrees from north. interval_max Maximum time interval belonging to a single profile in seconds. Traffic rates are set to zero at times t for which no profiles can be found within the period t-interval_max/2 to t+interval_max/2. Ignored for single profiles of class vp.

### Details

#### Available quantities

The function generates a specially classed data frame with the following quantities:

datetime

POSIXct date of each profile in UTC

vid

Vertically Integrated Density in individuals/km^2. vid is a surface density, whereas dens in vp objects is a volume density.

vir

Vertically Integrated Reflectivity in cm^2/km^2

mtr

Migration Traffic Rate in individuals/km/h

rtr

Reflectivity Traffic Rate in cm^2/km/h

mt

Migration Traffic in individuals/km, cumulated from the start of the time series up to datetime

rt

Reflectivity Traffic in cm^2/km, cumulated from the start of the time series up to datetime

ff

Horizontal ground speed in m/s

dd

Horizontal ground speed direction in degrees

u

Ground speed component west to east in m/s

v

Ground speed component north to south in m/s

height

Mean flight height (height weighted by eta) in m above sea level

Vertically integrated density and reflectivity are related according to vid=vir/rcs(x), with rcs the assumed radar cross section per individual. Similarly, migration traffic rate and reflectivity traffic rate are related according to mtr=rtr/rcs(x)

#### Ground speed (ff) and ground speed components (u,v)

The height-averaged ground speed is defined as:

ff = ∑_i dens_i ff_i / ∑_i dens_i

with the sum running over all altitude layers between alt_min and alt_max, dens_i the bird density, ff_i the ground speed at altitude layer i.

the height-averaged u component (west to east) is defined as:

u = ∑_i dens_i u_i / ∑_i dens_i

the height-averaged v component (south to north) is defined as:

v = ∑_i dens_i v_i / ∑_i dens_i

Note that ff_i=√(u_i^2 + v_i^2), but the same does not hold for the height-integrated speeds, i.e. ff != √(u^2 + v^2) as soon as the ground speed directions vary with altitude.

#### Migration traffic rate (mtr) and reflectivity traffic rate (rtr)

Migration traffic rate (mtr) for an altitude layer is a flux measure, defined as the number of targets crossing a unit of transect per hour.

Column mtr of the output dataframe gives migration traffic rates in individuals/km/hour.

The transect direction is set by the angle alpha. When alpha=NA, the transect runs perpendicular to the measured migratory direction. mtr then equals the number of crossing targets per km transect per hour, for a transect kept perpendicular to the measured migratory movement at all times and altitudes. In this case mtr is always a positive quantity, defined as:

mtr = 3.6 ∑_i dens_i ff_i Δ h

with the sum running over all altitude layers between alt_min and alt_max, dens_i the bird density, ff_i the ground speed at altitude layer i, and Δ h the altitude layer width. The factor 3.6 refers to a unit conversion of speeds ff_i from m/s to km/h.

If alpha is given a numeric value, the transect is taken perpendicular to the direction alpha, and the number of crossing targets per hour per km transect is calculated as:

mtr = 3.6 ∑_i dens_i ff_i \cos((dd_i-alpha) pi/180) Δ h

with dd_i the migratory direction at altitude i.

Note that this equation evaluates to the previous equation when alpha equals dd_i. Also note we can rewrite this equation using trigonemetry as:

mtr = 3.6 ∑_i dens_i (u_i \sin(alpha pi/180) + v_i \cos(alpha pi/180)) Δ h

with u_i and v_i the u and v ground speed components at altitude i.

In this definition mtr is a traditional flux into a direction of interest. Targets moving into the direction alpha contribute positively to mtr, while targets moving in the opposite direction contribute negatively to mtr. Therefore mtr can be both positive or negative, depending on the definition of alpha.

Note that mtr for a given value of alpha can also be calculated from the vertically integrated density vid and the height-integrated velocity components u and v as follows:

mtr = 3.6 (u \sin(alpha pi/180) + v \cos(alpha pi/180)) vid

Formula for reflectivity traffic rate rtr are found by replacing dens with eta and vid with vir in the formula for mtr. Reflectivity traffic rate gives the cross-sectional area passing the radar per km transect perpendicular to the migratory direction per hour. mtr values are conditional on settings of rcs, while rtr values are not.

#### Migration traffic (mt) and reflectivity traffic (rt)

Migration traffic is calculated by time-integration of migration traffic rates. Migration traffic gives the number of individuals that have passed per km perpendicular to the migratory direction at the position of the radar for the full period of the time series within the specified altitude band.

Reflectivity traffic is calculated by time-integration of reflectivity traffic rates. Reflectivity traffic gives the total cross-sectional area that has passed per km perpendicular to the migratory direction at the position of the radar for the full period of the time series within the specified altitude band.

mt values are conditional on settings of rcs, while rt values are not.

Columnns mt and rt in the output dataframe provides migration traffic as a numeric value equal to migration traffic and reflectivity traffic from the start of the time series up till the moment of the time stamp of the respective row.

### Value

an object of class vpi, a data frame with vertically integrated profile quantities

### Methods (by class)

• vp: Vertically integrate a vertical profile.

• list: Vertically integrate a list of vertical profiles.

• vpts: Vertically integrate a time series of vertical profiles.

### Examples

# MTR for a single vertical profile
integrate_profile(example_vp)

# MTRs for a list of vertical profiles
integrate_profile(c(example_vp, example_vp))

# MTRs for a time series of vertical profiles