Rainfall and climate variables used in the literature for the definition
of rainfall thresholds for the initiation of landslides. Table lists the
variable, the units of measure most commonly used for the parameter, and
the author(s) who first introduced the parameter. Nomenclature is not consistent
in the literature, and different definitions have been used for the same
or similar variables. |
VARIABLE |
DESCRIPTION |
UNITS |
FIRST INTRODUCED |
D |
Rainfall duration. The duration of the rainfall event or rainfall period. |
h, or days |
Caine (1980) |
DC |
Duration of the critical rainfall event. |
h |
Aleotti
(2004) |
E(h),(d) |
Cumulative
event rainfall. The total rainfall measured from the beginning
of the rainfall event to the time of failure. Also
known as storm rainfall. “h” indicates
the considered period in hours; “d” indicates the considered
period in days. |
mm |
Innes
(1983) |
EMAP |
Normalized cumulative event rainfall. Cumulative event rainfall divided
by MAP (EMAP=E/MAP). Also known as normalized storm rainfall. |
- |
Guidicini
and Iwasa (1977) |
C |
Critical rainfall. The total amount of rainfall from the time of a distinct
increase in rainfall intensity (t0) to the time of the triggering of the
first landslide (tf). |
mm |
Govi
and Sorzana (1980) |
CMAP |
Normalized critical rainfall. Critical rainfall divided by MAP (CMAP=C/MAP). |
- |
Govi
and Sorzana (1980) |
R |
Daily rainfall. The total amount of rainfall for the day of the landslide
event. |
mm |
Crozier
and Eyles (1980) |
RMAP |
Normalized daily rainfall. Daily rainfall divided by MAP (RMAP=R/MAP). |
mm |
Terlien
(1998) |
I |
Rainfall intensity. The amount of precipitation in a period, i.e., the
rate of precipitation over the considered period. Depending on the duration
of the measuring period, rainfall intensity measures peak or average precipitation
rates. |
mm/h |
Caine (1980) |
IMAP |
Normalized rainfall intensity. Rainfall intensity divided by MAP (IMAP=I/MAP). |
1/h |
Cannon
(1988) |
IMAX |
Maximum hourly rainfall intensity. The maximum hourly rainfall intensity. |
mm/h |
Onodera
et al. (1974) |
IP |
Peak rainfall intensity. The highest rainfall intensity (rainfall rate)
during a rainfall event. Available from detailed rainfall records. |
mm/h |
Wilson
et al. (1992) |
Î(h) |
Mean
rainfall intensity for final storm period. “h” indicates
the considered period, in hours, most commonly from 3 to 24 hours. |
mm/h |
Govi
and Sorzana (1980) |
IC |
Critical hourly rainfall intensity. |
mm/h |
Heyerdahl
et al. (2003) |
If |
Rainfall intensity at the time of the slope failure. Available from detailed
rainfall records. |
mm/h |
Aleotti
(2004) |
IfMAP |
Normalized rainfall intensity at the time of the slope failure. Rainfall
intensity at the time of the slope failure divided by MAP (IfMAP=If/MAP). |
1/h |
Aleotti
(2004) |
A(d) |
Antecedent
rainfall. The total (cumulative) precipitation measured before
the landslide triggering rainfall event. “d” indicates
the considered period in days. |
mm |
Govi
and Sorzana (1980) |
AMAP |
Normalized antecedent rainfall. Antecedent rainfall divided by MAP (AMAP=A/MAP). |
- |
Aleotti
(2004) |
A(y) |
Antecedent yearly precipitation up to date of the event. The total (cumulative)
yearly precipitation measured before the landslide triggering rainfall
event. |
mm |
Guidicini
and Iwasa (1977) |
A(y)MAP |
Normalized antecedent yearly precipitation up to date of the event. Antecedent
yearly precipitation divided by MAP (A(y)MAP=A(y)/MAP). |
- |
Guidicini
and Iwasa (1977) |
FC |
Sum
of normalized antecedent yearly precipitation and normalized event
rainfall (FC=A(y)MAP+EMAP). Also known as “final coefficient”. |
- |
Guidicini
and Iwasa (1977) |
MAP |
Mean annual precipitation. For a rain gauge, the long term yearly average
precipitation, obtained from historical rainfall records. A proxy for local
climatic conditions. |
mm |
Guidicini
and Iwasa (1977) |
RDs |
Average number of rainy-days in a year. For a rain gauge, the long term
yearly average of rainy (or wet) days, obtained from historical rainfall
records. A proxy for local climatic conditions. |
# |
Wilson
and Jayko (1997) |
RDN |
Rainy-day normal. For a rain gauge, the ratio between the MAP and the
average number of rainy-days in a year (RDN=MAP/RDs). |
mm/# |
Wilson
and Jayko (1997) |
N |
Ratio between the MAP of two different (distant) areas. |
- |
Barbero
at al. (2004) |
|