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Exploring Antarctic subglacial lakes with scientific probes: a formal probabilistic approach for operational risk management

Published online by Cambridge University Press:  08 September 2017

M.P. Brito
Affiliation:
National Oceanography Centre, University of Southampton, Southampton, UK. E-mail: mario.brito@noc.ac.uk
G. Griffiths
Affiliation:
National Oceanography Centre, University of Southampton, Southampton, UK. E-mail: mario.brito@noc.ac.uk
M. Mowlem
Affiliation:
National Oceanography Centre, University of Southampton, Southampton, UK. E-mail: mario.brito@noc.ac.uk
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Abstract

Since their discovery, Antarctic subglacial lakes have become of great interest to the science community. It is hypothesized that they may hold unique forms of biological life and that they hold detailed sedimentary records of past climate change. According to the latest inventory, a total of 387 subglacial lakes have been identified in Antarctica (Wright and Siegert, 2011). However, exploration using scientific probes has yet to be performed. We propose a generic, formal approach to manage the operational risk of deploying probes during clean access to subglacial lake exploration. A representation of the entire probe deployment process is captured in a Markov chain. The transition from one state to the next depends on several factors, including reliability of components and processes. We use fault trees to quantify the probability of failure of the complex processes that must take place to facilitate the transition from one state to another. Therefore, the formal framework consists of integrating a Markov chain, fault trees, component and subsystem reliability data and expert judgment. To illustrate its application we describe how the approach can be used to address a series of what-if scenarios, using the intended Ellsworth Subglacial Lake probe deployment as a case study.

Information

Type
Instruments and Methods
Copyright
Copyright © International Glaciological Society 2012
Figure 0

Fig. 1. Three-dimensional computer-aided design (CAD) rendering of the Ellsworth Subglacial Lake probe concept which consists of two gas- filled pressure cases separated by three carousels of water samplers and filters, all attached to a central core that is attached to the tether.

Figure 1

Fig. 2. Markov state space model capturing the sequence of events undertaken during the Ellsworth probe design and deployment.

Figure 2

Table 1. Discrete states from the state diagram presented in Figure 2

Figure 3

Table 2. Notation and conditions for the Markov model in Figure 2. pi, j is the transition probability from state i to state j

Figure 4

Fig. 3. Fault tree used for deriving transition probability p10,11. Thirty-three base events are shown; the probability of failure for each base event is the 95% quantile of the agreed assessment. The probability pf10 stands for failure to complete phase 10.

Figure 5

Fig. 4. Probability of failure cumulative distribution for (a) the first-level failure modes in the fault tree of Figure 3 and (b) the second-level

Figure 6

Fig. 5. Expert judgments for the top ten most critical failure modes: (a) tether handling failure; (b) communication optical connector failure; (c) design failure during sheave deployment; (d) handling of the sheave; (e) tether handling failure caused by bag damage during systems predeployment test; (f) tether handling failure caused by bag damage during systems pre-deployment test; (g) tether electronic connector failure during systems pre-deployment test; (h) polythene failure during sheave deployment; (i) topside systems failure due to human error during systems pre-deployment tests; (j) electronics sensor failure, i.e. at least one sensor fails, during pre-deployment systems test.

Figure 7

Fig. 5.

Figure 8

Fig. 6. Markov state space model capturing the sequence of events undertaken during the Ellsworth probe design and deployment.