Arbeitspapier

Identifying credit supply shocks with bank-firm data: Methods and applications

Current empirical methods to identify and assess the impact of bank credit supply shocks rely strictly on multi-bank firms and ignore firms borrowing from only one bank. Yet, these single-bank firms are often the majority of firms in an economy and most prone to credit supply shocks. We propose and underpin an alternative demand control (using industry-location-size-time fixed effects) that allows identifying timevarying cross-sectional bank credit supply shocks using both single- and multi-bank firms. Using matched bank-firm credit data from Belgium, we show that firms borrowing from banks with negative credit supply shocks exhibit lower financial debt growth, asset growth, investments, and operating margin growth. Positive credit supply shocks are associated with bank risk-taking behaviour at the extensive margin. Importantly, to capture these effects it is crucial to include the single-bank firms when identifying the bank credit supply shocks.

Language
Englisch

Bibliographic citation
Series: NBB Working Paper ; No. 347

Classification
Wirtschaft
Banks; Depository Institutions; Micro Finance Institutions; Mortgages
Financing Policy; Financial Risk and Risk Management; Capital and Ownership Structure; Value of Firms; Goodwill
Subject
credit supply identification
bank lending
corporate investment
bank risk-taking

Event
Geistige Schöpfung
(who)
Degryse, Hans
De Jonghe, Olivier
Jakovljević, Sanja
Mulier, Klaas
Schepens, Glenn
Event
Veröffentlichung
(who)
National Bank of Belgium
(where)
Brussels
(when)
2018

Handle
Last update
10.03.2025, 11:45 AM CET

Data provider

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ZBW - Deutsche Zentralbibliothek für Wirtschaftswissenschaften - Leibniz-Informationszentrum Wirtschaft. If you have any questions about the object, please contact the data provider.

Object type

  • Arbeitspapier

Associated

  • Degryse, Hans
  • De Jonghe, Olivier
  • Jakovljević, Sanja
  • Mulier, Klaas
  • Schepens, Glenn
  • National Bank of Belgium

Time of origin

  • 2018

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