information flows, etc. Within the loosely coupled 
system, process architecture is subjected to dynamic 
change, due to frequent and spontaneous interaction 
among entities, information flows, and process 
patterns. Consequently, there is no guarantee to 
foretell, how the final process model will settle and 
make process execution possible. Taking in the 
consideration haste of the system`s emergence and its 
short-term operation, such system evolves with a 
tendency to reach a desired process output and 
afterwards disintegrates into few tight organizational 
systems. 
Niu (2010) advocates the significance and the 
influence in the relation between the knowledge and 
the system`s adaptation. According to Martinez-Leon 
and Martinez-Garcia (2011) less formal and less 
centralized organizational systems enhances the 
organizational learning process. Open, less rigid, 
loosely coupled organizational system on the one 
hand creates an open environment that encourages 
organizational learning, but on the other hand creates 
also a need to assess more complex, less transparent 
and harder to follow learning process. Tennant and 
Fernie (2013) found learning within the loosely 
coupled system similar to the underdeveloped 
knowledge management approach in the industrial 
enterprises. In both cases, learning adapted to the 
process and changed with activity flows in a 
reactionary and interventionary manner. Firestone 
and McElroy (2004) argue that rapid change in the 
process architecture not only boosts new variants of 
work processes, but also learning processes and 
processes for managing knowledge.  
Even though several authors detected and 
described learning processes within the loosely 
coupled system, we found no tangible and wide 
knowledge interaction within the assessed flood 
response system. We detected two different learning 
processes with no traceable interaction. First learning 
process occurs within formal and tight subsystems in 
the loosely coupled system. Learning takes place 
within the scope of the subsystem before its 
integration into the overall flood response system. 
The knowledge gained through such a learning 
process is explicit, specific and differs on the kind of 
the learning subsystem. No traceable interchange 
among entities with such knowledge or other entities 
is detected. Second learning process occurs when the 
flood endangered communities face direct flood 
threat. They are subjected to the experiential learning, 
emerging tacit knowledge about one or several 
floods. There is no traceable knowledge interchange 
among flood-endangered communities and among 
other entities, as well. 
Even though the Resolution of national security 
strategy of the Republic of Slovenia (2010) and the 
Resolution of the national program of protection 
against natural and other disasters from year 2009 to 
year 2015 (2009), contain guidelines which would 
practically establish knowledge interchange between 
both groups, no such attempt has been recorded yet.  
Implementation of a knowledge interchange 
mechanism would on the first hand enabled the 
smooth transfer of the knowledge among different 
entities within the system, and on the other hand, it 
would significantly optimize the flood response 
process, executed by the loosely coupled system. 
3 BACKGROUND 
INFORMATION 
To be able to understand how communities in the 
flood response system perceived floods and how they 
learned from them and about them, we collected 
general information about the flood threatened area, 
together with hydrological and meteorological data, 
describing all 4 floods. 
3.1 General Information 
A good part of a Lower Sava region occupies Krško-
Brežice field, which is a valley, surrounded by 
Gorjanci Hills on the southern side and Posavje hills 
on the northern side. Two bigger municipalities 
(Krško and Brežice) are situated in the valley and one 
smaller (Kostanjevica na Krki). There are five flood 
sources in the valley. In addition to the Sava and the 
Krka, as two major rivers, the streams that carry water 
from the hills quickly grow into torrents with a 
threatening power within few days of continuous rain. 
The rain itself can cause considerable problems when 
meteoric water starts to overwhelm the low 
positioned planes with impermeable soil layers. The 
communities and the infrastructure located low and 
near the river can experience groundwater flooding, 
which usually affects the underground parts of 
buildings, such as basements, engine rooms, garages, 
workshops, etc. 
According to the Department for hydrological 
prognosis of the Slovenian environmental agency 
(2012), flooding of the Krka River in the 
communities, in the municipality of Brežice, which 
are located within the 8 km area before the confluence 
with the Sava River, is highly dependent on the Sava 
River and its flow rate. High flow rates of the Krka 
River alone represent a threat to the western