How much do bank shocks affect investment? Evidence from matched bank-firm loan data
Mary Amiti and
David Weinstein
No 604, Staff Reports from Federal Reserve Bank of New York
Abstract:
We show that supply-side financial shocks have a large impact on firms' investment. We do this by developing a new methodology to separate firm-borrowing shocks from bank supply shocks using a vast sample of matched bank-firm lending data. We decompose loan movements in Japan for the period 1990 to 2010 into bank, firm, industry, and common shocks. The high degree of financial institution concentration means that individual banks are large relative to the size of the economy, which creates a role for granular shocks as in Gabaix (2011). As a result, bank supply shocks?that is, movements in the supply of bank loans net of borrower characteristics and general credit conditions?can have large impacts on aggregate loan supply and investment. We show that these bank supply shocks explain 40 percent of aggregate loan and investment fluctuations.
Keywords: credit constraints; investment (search for similar items in EconPapers)
JEL-codes: E44 G21 (search for similar items in EconPapers)
Date: 2013-03-01
References: View references in EconPapers View complete reference list from CitEc
Citations: View citations in EconPapers (37)
Downloads: (external link)
https://www.newyorkfed.org/medialibrary/media/research/staff_reports/sr604.pdf (application/pdf)
Related works:
Working Paper: How Much do Bank Shocks Affect Investment? Evidence from Matched Bank-Firm Loan Data (2013) 
This item may be available elsewhere in EconPapers: Search for items with the same title.
Export reference: BibTeX
RIS (EndNote, ProCite, RefMan)
HTML/Text
Persistent link: https://EconPapers.repec.org/RePEc:fip:fednsr:604
Ordering information: This working paper can be ordered from
Access Statistics for this paper
More papers in Staff Reports from Federal Reserve Bank of New York Contact information at EDIRC.
Bibliographic data for series maintained by Gabriella Bucciarelli ().