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Journal articles on the topic 'Balance sheet'

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Published: 4 June 2021
Last updated: 11 March 2023

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1

Lloyd, John. "A balance sheet." Index on Censorship 25, no. 3 (May 1996): 48–53. http://dx.doi.org/10.1080/03064229608536074.

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2

Kiyotaki, Nobuhiro, and John Moore. "Balance-Sheet Contagion." American Economic Review 92, no. 2 (April 1, 2002): 46–50. http://dx.doi.org/10.1257/000282802320188989.

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3

Mingalev, Oleg, Pavel Setsko, Mikhail Melnik, Igor Mingalev, Helmi Malova, and Alexey Merzlyi. "Force balance in current sheets in collisionless plasma." Solar-Terrestrial Physics 7, no. 2 (June 30, 2021): 11–21. http://dx.doi.org/10.12737/stp-72202102.

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In this paper, we derive a divergent form of the force balance equation for collisionless plasma in the quasineutrality approximation, in which the electric field and current density are excluded. For a stationary spatially one-dimensional current sheet with a constant normal component of the magnetic field and magnetized electrons, the general form of the force balance equation has been obtained for the first time in the form of a conservation law. An equation in this form is necessary for the correct formulation of boundary conditions when modeling asymmetric current sheets, as well as for the control of the stationarity of the numerical solution obtained in the model. Furthermore, the fulfillment of this equation is considered for two types of stationary configurations of a thin current sheet, which are obtained using a numerical model. The derived equation makes it possible to develop models of asymmetric current sheets, in particular current sheets on the magnetopause flanks in the magnetotail.
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4

Rahman, Asheq, Hector Perera, and Frances Chua. "Asia Pulp & Paper: a balanced balance sheet?" Emerald Emerging Markets Case Studies 6, no. 3 (November 23, 2016): 1–26. http://dx.doi.org/10.1108/eemcs-05-2015-0095.

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Subject area International business, Accounting and Finance. Study level/applicability Undergraduate and Postgraduate levels (advanced financial accounting, international accounting, other accounting and business courses with an international setting. Case overview The case uses the Asia Pulp & Paper Company’s (APP) entry into the international debt market to highlight the consequences of different business practices between the East (in this case, Indonesia) and the West. On the one hand, it shows that APP was set up as the “front” to access international debt capital; on the other, it reveals the naïvety of Western lenders who parted with their funds without conducting a thorough background research on the financial viability of the company they invested in. The APP debacle is a poignant reminder for market participants and business/accounting students that the divergence of the business settings across countries can make business contractual arrangements tenuous and corporate financial information irrelevant to its users. It also exposes the unique ways of how some Asian countries conduct their business affairs. Expected learning outcomes The following are the expected learning outcomes: comprehend the impact of differences in culture and ethnic origin on business practices; evaluate the impact of cultural nuances on the legality of contracts in the international business setting; understand the impact of currency fluctuation on the financial position of multinational firms; and be more cautious in conducting business and entering into contracts with foreign firms. Supplementary materials Teaching notes are available for educators only. Please contact your library to gain login details or email support@emeraldinsight.com to request teaching notes. Subject code CCS 1: Accounting and Finance.
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5

Adams, Nicholas. "JSAH: A Balance Sheet." Journal of the Society of Architectural Historians 56, no. 1 (March 1, 1997): 4–5. http://dx.doi.org/10.2307/991212.

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6

Hunter, Shireen T. "Terrrorism: A Balance Sheet." Washington Quarterly 12, no. 3 (June 1989): 17–29. http://dx.doi.org/10.1080/01636608909477514.

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7

Weetman, Pauline. "Off-balance sheet financing." British Accounting Review 21, no. 1 (March 1989): 103–5. http://dx.doi.org/10.1016/0890-8389(89)90084-x.

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8

DICKS, GEOFFREY, and MELANIE ROBERTS. "The UK Balance Sheet." Economic Outlook 11, no. 9 (June 1987): 26–33. http://dx.doi.org/10.1111/j.1468-0319.1987.tb00656.x.

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9

Weale, Martin. "The national balance sheet." National Institute Economic Review 184 (April 2003): 43–44. http://dx.doi.org/10.1177/002795010318400105.

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Discussion around the time of the budget focuses on the state of the Government's finances, both in terms of the balance of income and expenditure, and also on their implications for the government balance sheet. Despite the wide-ranging nature of some of the budget commentary, the issue of the national balance sheet received no discussion there and attracts little attention generally.
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10

Binder, D. "A Balkan Balance Sheet." Mediterranean Quarterly 11, no. 1 (January 1, 2000): 49–54. http://dx.doi.org/10.1215/10474552-11-1-49.

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11

Koonce, Lisa, Zheng Leitter, and Brian J. White. "Linked balance sheet presentation." Journal of Accounting and Economics 68, no. 1 (August 2019): 101237. http://dx.doi.org/10.1016/j.jacceco.2019.101237.

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12

Thompson, Starley L., and David Pollard. "Ice-sheet mass balance at the Last Glacial Maximum from the GENESIS version 2 global climate model." Annals of Glaciology 25 (1997): 250–58. http://dx.doi.org/10.3189/s0260305500268109.

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AbstractAt the Last Glacial Maximum (LGM) about 21000 years ago (21 ka BP), the overall mass balance of the Laurentide and Eurasian ice sheets should have been close to zero, since their rate of change of total ice volume was approximately zero at that time. The surface mass balance should have been zero or positive to balance any iceberg/iceshelf discharge and basal melting, but could not have been strongly negative. In principle this can be tested by global climate model (GCM) simulations with prescribed ice-sheet extents and topography.We describe results from a suite of 21 ka BP simulations using a new GCM (GENESIS version 2.0.a), with sea-surface temperatures (SSTs) prescribed from GLIMAP (1981) and predicted by a mixed-layer ocean model, and with ice sheets prescribed from both the ICE-4G (Peltier, 1994) and CLIMAP (1981) reconstructions. This GCM is well suited for ice-sheet mass-balance studies because (i) the surface can be represented at a finer resolution than the atmospheric GCM, (ii) an elevation correction accounts for spectral distortions of the atmospheric GCM topography, (iii) a simple post-processing correction for the refreezing of meltwater is applied, and (iv) the model's precipitation and mass balances for present-day Greenland and Antarctica are realistic. However, for all reasonable combinations of SSTs and ice-sheet configurations, the predicted annual surface mass balances of the LGM Laurentide and Eurasian ice sheets are implausibly negative. Possible reasons for this discrepancy are discussed, including increased ice-age aerosols, higher CLIMAP-like ice-sheet profiles in the few thousand years preceding the LGM, and a surface of the southern Laurentide just before the LGM to produce fleetingly the ICE-4G profile at 21 ka BP.
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13

Trufanov, Yu S. "Development of automated balance flow-sheets in refinery commodity and feedstock depots." Herald of Dagestan State Technical University. Technical Sciences 48, no. 2 (July 31, 2021): 50–59. http://dx.doi.org/10.21822/2073-6185-2021-48-2-50-59.

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Objective. Development of automated balance flow-sheets in commodity and feedstock depots. Methods. Methods for modelling balance flow-sheets of commodity and feedstock depots, taking into account petroleum products movement and shipping plans, were applied. Results. Examples of automated balance flow-sheets of commodity and feedstock depots specific to refineries are given with the description of technological processes or oil product shipment processes. Rail, road, water, and pipelines shipment automation processes are shown. Operational and daily summaries of balance objects, such as a tank or a group of tanks (commodity group), are graphically shown. An example of an automated dispatch sheet formed on the basis of corresponding automated balance flow-sheets is given. Conclusion. The implementation of automated flow-sheets for all significant production facilities at a refinery, in particular for commodity and feedstock depots, will ensure the visibility and transparency of information on balance objects, which is subsequently used to close a balance sheet for the enterprise as a whole.
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14

Ramstein, Gilles, Adeline Fabre, Sophie Pinot, Catherine Ritz, and Sylvie Joussaume. "Ice-sheet mass balance during the last glacial maximum." Annals of Glaciology 25 (1997): 145–52. http://dx.doi.org/10.3189/s026030550001394x.

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In the framework of the Paleoclimate Modelling Intercomparison Project (PMIP), simulations of the Last Glacial Maximum (LGM) have- been performed. More than 10 different atmospheric general circulation models (AGCMs) have been used with the same boundary conditions: sea-surface temperatures prescribed by CLIMAP (1981), ice-sheet reconstruction provided by Peltier (1994), change in insolation, and reduced CO2 content. One of the major questions is to investigate whether the simulations of the LGM are in equilibrium with the prescribed ice-sheet reconstruction. To answer this question, we have used two different approaches. First, we analyze the results of a sel of LGM simulations performed with different versions of the Laboratoire de Meteorolo-gie Dynamique (LMD) AGCM and study the hydrologic and snow- budgets over the Laurcntide and Fennoscandian ice sheets. Second, we use the AGCM outputs to force an ice-sheet model in order to investigate its ability to maintain the ice sheets as reconstructed by CLIMAP (1981) or Peltier (1994).
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15

Ramstein, Gilles, Adeline Fabre, Sophie Pinot, Catherine Ritz, and Sylvie Joussaume. "Ice-sheet mass balance during the last glacial maximum." Annals of Glaciology 25 (1997): 145–52. http://dx.doi.org/10.1017/s026030550001394x.

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In the framework of the Paleoclimate Modelling Intercomparison Project (PMIP), simulations of the Last Glacial Maximum (LGM) have- been performed. More than 10 different atmospheric general circulation models (AGCMs) have been used with the same boundary conditions: sea-surface temperatures prescribed by CLIMAP (1981), ice-sheet reconstruction provided by Peltier (1994), change in insolation, and reduced CO2 content. One of the major questions is to investigate whether the simulations of the LGM are in equilibrium with the prescribed ice-sheet reconstruction. To answer this question, we have used two different approaches. First, we analyze the results of a sel of LGM simulations performed with different versions of the Laboratoire de Meteorolo-gie Dynamique (LMD) AGCM and study the hydrologic and snow- budgets over the Laurcntide and Fennoscandian ice sheets. Second, we use the AGCM outputs to force an ice-sheet model in order to investigate its ability to maintain the ice sheets as reconstructed by CLIMAP (1981) or Peltier (1994).
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16

Plach, Andreas, Kerim H. Nisancioglu, Petra M. Langebroek, Andreas Born, and Sébastien Le clec'h. "Eemian Greenland ice sheet simulated with a higher-order model shows strong sensitivity to surface mass balance forcing." Cryosphere 13, no. 8 (August 15, 2019): 2133–48. http://dx.doi.org/10.5194/tc-13-2133-2019.

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Abstract. The Greenland ice sheet contributes increasingly to global sea level rise. Its history during past warm intervals is a valuable reference for future sea level projections. We present ice sheet simulations for the Eemian interglacial period (∼130 000 to 115 000 years ago), a period with warmer-than-present summer climate over Greenland. The evolution of the Eemian Greenland ice sheet is simulated with a 3-D higher-order ice sheet model, forced with a surface mass balance derived from regional climate simulations. Sensitivity experiments with various surface mass balances, basal friction, and ice flow approximations are discussed. The surface mass balance forcing is identified as the controlling factor setting the minimum in Eemian ice volume, emphasizing the importance of a reliable surface mass balance model. Furthermore, the results indicate that the surface mass balance forcing is more important than the representation of ice flow for simulating the large-scale ice sheet evolution. This implies that modeling of the future contribution of the Greenland ice sheet to sea level rise highly depends on an accurate surface mass balance.
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17

Malloy, Matthew, Francis Martinez, Mary-Frances Styczynski, and Alex Thorp. "Retail CBDC and U.S. Monetary Policy Implementation: A Stylized Balance Sheet Analysis." Finance and Economics Discussion Series 2022, no. 032 (May 31, 2022): 1–17. http://dx.doi.org/10.17016/feds.2022.032.

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This paper discusses how a Federal Reserve issued retail central bank digital currency (CBDC) could affect U.S. monetary policy implementation. Using a stylized balance sheet analysis, we analyze the effect a retail CBDC could have on the balance sheets of the Federal Reserve, commercial banks, and U.S. households. Then we consider how these balance sheet changes could affect monetary policy implementation for the Federal Reserve. We illustrate that the potential effects on monetary policy implementation from a retail CBDC are highly dependent on the initial conditions of the Federal Reserve’s balance sheet. Moreover, the analysis demonstrates how the Federal Reserve may use its existing tools to manage the effects of a retail CBDC on monetary policy implementation.
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18

Kirschenbaum, Jill. "Auditing the Environmental Balance Sheet." Business Ethics: The Magazine of Corporate Responsibility 4, no. 5 (1990): 13–14. http://dx.doi.org/10.5840/bemag19904544.

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19

Flynn, James R. "Male and Female Balance Sheet." Mankind Quarterly 58, no. 1 (2017): 43–68. http://dx.doi.org/10.46469/mq.2017.58.1.3.

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20

Thies, Clifford F., and Thomas Sturrock. "The Pension-Augmented Balance Sheet." Journal of Risk and Insurance 55, no. 3 (September 1988): 467. http://dx.doi.org/10.2307/253255.

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21

Young, Crawford. "Africa: An Interim Balance Sheet." Journal of Democracy 7, no. 3 (1996): 53–68. http://dx.doi.org/10.1353/jod.1996.0053.

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22

Horan, Stephen M. "Measuring Off-Balance-Sheet Leverage." CFA Digest 32, no. 3 (August 2002): 99. http://dx.doi.org/10.2469/dig.v32.n3.1143.

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23

Breuer, Peter. "Measuring off-Balance-Sheet Leverage." IMF Working Papers 00, no. 202 (2000): i. http://dx.doi.org/10.5089/9781451874396.001.

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24

Chin, G. J. "BIOTECHNOLOGY: Improving the Balance Sheet." Science 316, no. 5824 (April 27, 2007): 516b. http://dx.doi.org/10.1126/science.316.5824.516b.

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25

O'Donoghue, Jim. "The public sector balance sheet." Economic & Labour Market Review 3, no. 7 (July 2009): 37–42. http://dx.doi.org/10.1057/elmr.2009.125.

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26

Aspinall, R., and P. Gregory. "Ecosystem Services: Nature's Balance Sheet." Science 342, no. 6157 (October 24, 2013): 421. http://dx.doi.org/10.1126/science.342.6157.421-a.

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27

Cabezon, Ezequiel, and Christian Henn. "Norway’s public sector balance sheet." Applied Economics Letters 27, no. 11 (July 29, 2019): 930–36. http://dx.doi.org/10.1080/13504851.2019.1646865.

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28

Breuer, Peter. "Measuring off-balance-sheet leverage." Journal of Banking & Finance 26, no. 2-3 (March 2002): 223–42. http://dx.doi.org/10.1016/s0378-4266(01)00220-5.

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29

Mills, Karen, Steven Morling, and Warren Tease. "Balance Sheet Restructuring and Investment." Australian Economic Review 27, no. 1 (January 1994): 83–100. http://dx.doi.org/10.1111/j.1467-8462.1994.tb00826.x.

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30

Adrian, Tobias, and Hyun Song Shin. "Financial Intermediary Balance Sheet Management." Annual Review of Financial Economics 3, no. 1 (December 2011): 289–307. http://dx.doi.org/10.1146/annurev-financial-102710-144915.

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31

Brzoska, Michael. "Military Conversion: The Balance Sheet." Journal of Peace Research 36, no. 2 (March 1999): 131–40. http://dx.doi.org/10.1177/0022343399036002001.

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32

FRIEDMAN, MILTON. "SAVINGS AND THE BALANCE SHEET." Bulletin of the Oxford University Institute of Economics & Statistics 19, no. 2 (May 1, 2009): 125–36. http://dx.doi.org/10.1111/j.1468-0084.1957.mp19002003.x.

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33

Sandri, Damiano, and Fabian Valencia. "Balance-Sheet Shocks and Recapitalizations." IMF Working Papers 12, no. 68 (2012): 1. http://dx.doi.org/10.5089/9781463938451.001.

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34

Brede, Maren, and Christian Henn. "Finland’s public sector balance sheet." Baltic Journal of Economics 19, no. 1 (January 2, 2019): 176–94. http://dx.doi.org/10.1080/1406099x.2019.1585062.

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35

Rémy, Frédérique, and Massimo Frezzotti. "Antarctica ice sheet mass balance." Comptes Rendus Geoscience 338, no. 14-15 (November 2006): 1084–97. http://dx.doi.org/10.1016/j.crte.2006.05.009.

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36

Fleckenstein, Matthias, and Francis A. Longstaff. "Renting Balance Sheet Space: Intermediary Balance Sheet Rental Costs and the Valuation of Derivatives." Review of Financial Studies 33, no. 11 (March 16, 2020): 5051–91. http://dx.doi.org/10.1093/rfs/hhaa033.

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Abstract A long-standing asset pricing puzzle is that the funding rates in derivatives contracts often differ from those in cash markets. We propose that the cost of renting intermediary balance sheet space may help resolve this puzzle. We study a persistent basis in what is arguably the largest derivatives market, namely, the interest rate futures market. This basis is strongly related to exogenous measures of intermediary balance sheet usage and proxies for the balance sheet costs imposed by debt overhang problems and capital regulation. These results extend to the cash derivatives bases documented in many of the other largest financial markets.
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37

Kachur, Iryna, Volodymyr Lepushynskyi, and Robert Zammit. "The NBU’s Balance Sheet: before, during, and after the Crisis." Visnyk of the National Bank of Ukraine, no. 237 (September 29, 2016): 6–19. http://dx.doi.org/10.26531/vnbu2016.237.006.

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Looking at the evolution of the central bank’s balance sheet gives us a unique window on the forces that have shaped our economy and central bank reaction functions. This paper considers the evolution of the NBU’s balance sheet over the period from 2001-2016, focusing on explicit and implicit monetary policy priorities at different periods. We then make simulations on the NBU’s balance sheet for the next five years assuming current NBU priorities for monetary policy. We then draw conclusions on the likely financial position of the NBU in the future and recommendations to ensure the NBU’s financial strength – essential for its continued independence.
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38

Mingalev, Oleg, Pavel Setsko, Mikhail Melnik, Igor Mingalev, Helmi Malova, and Alexey Merzlyi. "Force balance in current sheets in collisionless plasma." Solnechno-Zemnaya Fizika 7, no. 2 (June 30, 2021): 12–23. http://dx.doi.org/10.12737/szf-72202102.

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In this paper, we derive a divergent form of the force balance equation for collisionless plasma in the quasineutrality approximation, in which the electric field and current density are excluded. For a stationary spatially one-dimensional current sheet with a constant normal component of the magnetic field and magnetized electrons, the general form of the force balance equation has been obtained for the first time in the form of a conservation law. An equation in this form is necessary for the correct formulation of boundary conditions when modeling asymmetric current sheets, as well as for the control of the stationarity of the numerical solution obtained in the model. Furthermore, the fulfillment of this equation is considered for two types of stationary configurations of a thin current sheet, which are obtained using a numerical model. The derived equation makes it possible to develop models of asymmetric current sheets, in particular current sheets on the magnetopause flanks in the magnetotail.
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39

Allison, I., R. B. Alley, H. A. Fricker, R. H. Thomas, and R. C. Warner. "Ice sheet mass balance and sea level." Antarctic Science 21, no. 5 (October 2009): 413–26. http://dx.doi.org/10.1017/s0954102009990137.

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AbstractDetermining the mass balance of the Greenland and Antarctic ice sheets (GIS and AIS) has long been a major challenge for polar science. But until recent advances in measurement technology, the uncertainty in ice sheet mass balance estimates was greater than any net contribution to sea level change. The Fourth Assessment Report of the Intergovernmental Panel on Climate Change (AR4) was able, for the first time, to conclude that, taken together, the GIS and AIS have probably been contributing to sea level rise over the period 1993–2003 at an average rate estimated at 0.4 mm yr-1. Since the cut-off date for work included in AR4, a number of further studies of the mass balance of GIS and AIS have been made using satellite altimetry, satellite gravity measurements and estimates of mass influx and discharge using a variety of techniques. Overall, these studies reinforce the conclusion that the ice sheets are contributing to present sea level rise, and suggest that the rate of loss from GIS has recently increased. The largest unknown in the projections of sea level rise over the next century is the potential for rapid dynamic collapse of ice sheets.
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40

Mordret, Aurélien, T. Dylan Mikesell, Christopher Harig, Bradley P. Lipovsky, and Germán A. Prieto. "Monitoring southwest Greenland’s ice sheet melt with ambient seismic noise." Science Advances 2, no. 5 (May 2016): e1501538. http://dx.doi.org/10.1126/sciadv.1501538.

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The Greenland ice sheet presently accounts for ~70% of global ice sheet mass loss. Because this mass loss is associated with sea-level rise at a rate of 0.7 mm/year, the development of improved monitoring techniques to observe ongoing changes in ice sheet mass balance is of paramount concern. Spaceborne mass balance techniques are commonly used; however, they are inadequate for many purposes because of their low spatial and/or temporal resolution. We demonstrate that small variations in seismic wave speed in Earth’s crust, as measured with the correlation of seismic noise, may be used to infer seasonal ice sheet mass balance. Seasonal loading and unloading of glacial mass induces strain in the crust, and these strains then result in seismic velocity changes due to poroelastic processes. Our method provides a new and independent way of monitoring (in near real time) ice sheet mass balance, yielding new constraints on ice sheet evolution and its contribution to global sea-level changes. An increased number of seismic stations in the vicinity of ice sheets will enhance our ability to create detailed space-time records of ice mass variations.
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41

Payne, Antony, and David Sugden. "Climate and the Initiation of Maritime Ice Sheets." Annals of Glaciology 14 (1990): 232–37. http://dx.doi.org/10.3189/s026030550000865x.

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The lower latitude extension of polar water during Quaternary glaciations has two opposing effects on the mass balances of adjacent maritime ice sheets. Cooler air temperatures reduce ablation and increase the fraction of precipitation falling as snow, but also lead to reduced atmospheric moisture content and reduced precipitation. The effects of these contrasting processes on ice-sheet initiation are investigated using a coupled ice-sheet-atmospheric moisture model of the Loch Lomond ice sheet in Scotland (10 000 a B.P.). There is a delicate balance between the degree of cooling required to initiate ice accumulation and that which restricts the flow of moisture over the area. At the regional scale of Scotland, the combined effects of orographic enhancement and the inherent feedback between the rising ice-surface elevation and increasing mass balance are dominant, and ice-sheet growth accelerates. Comparison of the results from models using different wind directions suggests that south-westerly winds were prevalent during the Loch Lomond glaciation in contrast to the dominant westerly winds of the present day. The modelling experiments demonstrate the sensitivity and complexity of the links between ocean surface cooling and ice-sheet growth, particularly at the early stages of a glacial cycle.
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42

Payne, Antony, and David Sugden. "Climate and the Initiation of Maritime Ice Sheets." Annals of Glaciology 14 (1990): 232–37. http://dx.doi.org/10.1017/s026030550000865x.

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The lower latitude extension of polar water during Quaternary glaciations has two opposing effects on the mass balances of adjacent maritime ice sheets. Cooler air temperatures reduce ablation and increase the fraction of precipitation falling as snow, but also lead to reduced atmospheric moisture content and reduced precipitation. The effects of these contrasting processes on ice-sheet initiation are investigated using a coupled ice-sheet-atmospheric moisture model of the Loch Lomond ice sheet in Scotland (10 000 a B.P.). There is a delicate balance between the degree of cooling required to initiate ice accumulation and that which restricts the flow of moisture over the area. At the regional scale of Scotland, the combined effects of orographic enhancement and the inherent feedback between the rising ice-surface elevation and increasing mass balance are dominant, and ice-sheet growth accelerates. Comparison of the results from models using different wind directions suggests that south-westerly winds were prevalent during the Loch Lomond glaciation in contrast to the dominant westerly winds of the present day. The modelling experiments demonstrate the sensitivity and complexity of the links between ocean surface cooling and ice-sheet growth, particularly at the early stages of a glacial cycle.
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43

GĂDĂU, Liana. "The transposition of the balance sheet to financial and functional balance sheet. Research and development." Annals of "Spiru Haret". Economic Series 15, no. 3 (September 30, 2015): 21. http://dx.doi.org/10.26458/1532.

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As the title suggests, through this paper we want to highlight the necessity of treating again the content and the form of the balance sheet in order to adapt it to a more efficient analysis, this way surpassing the informational valences of the classic balance sheet.The functional and the financial balance sheet will be taken into account. These models of balance sheet permit the complex analyses regarding the solvability or the bankruptcy risk of an enterprise to take place, and also other analyses, like the analysis of the structure and the financial/ functional equilibrium, the analysis of the company on operating cycles and their role in the functioning of the company. Through the particularities offered by each of these two models of balance sheet, we want to present the advantages of a superior informing. This content of this material is based on a vast investigation of the specialized literature.
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44

"Balance Sheet." Astronomy & Geophysics 38, no. 5 (October 1, 1997): 37. http://dx.doi.org/10.1093/astrog/38.5.37.

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45

"Balance Sheet." Quarterly Journal of the Royal Meteorological Society 6, no. 34 (July 6, 2007): 67–70. http://dx.doi.org/10.1002/qj.4970063406.

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46

"Financial Balance Sheet." Financial Statistics 567, no. 1 (July 2009): 198–228. http://dx.doi.org/10.1057/fs.2009.100.

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47

"Financial Balance Sheet." Financial Statistics 568, no. 1 (August 2009): 198–228. http://dx.doi.org/10.1057/fs.2009.115.

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48

"Financial Balance Sheet." Financial Statistics 561, no. 1 (January 2009): 198–228. http://dx.doi.org/10.1057/fs.2009.13.

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49

"Financial Balance Sheet." Financial Statistics 569, no. 1 (September 2009): 198–228. http://dx.doi.org/10.1057/fs.2009.130.

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"Financial Balance Sheet." Financial Statistics 570, no. 1 (October 2009): 198–228. http://dx.doi.org/10.1057/fs.2009.145.

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