Changes in daily extreme temperatures in the extra‐Carpathians regions of Romania

Croitoru, Adina‐Eliza; Piticar, Adrian

doi:10.1002/joc.3567

Cited by 72 publications

(62 citation statements)

References 52 publications

Supporting

Mentioning

Contrasting

Unclassified

Order By: Relevance

“…Presented results are in line with previously published research indicating an increase of Bhot^extremes for the whole Europe (Yan et al 2002), as well as for regions and particular countries (Croitoru and Piticar 2012, El Kenawy et al 2011, Hundecha and Bardossy 2005. These studies dealt with time series of records commencing in the mid-twentieth century Konnen 2003, Nemec et al 2013) and earlier (Moberg and Jones 2005).…”

Section: Discussionsupporting

confidence: 90%

The heat goes on—changes in indices of hot extremes in Poland

Graczyk

Pińskwar

Kundzewicz

et al. 2016

Theor Appl Climatol

View full text Add to dashboard Cite

On the basis of temperature observations at 60 meteorological stations in Poland, changes in the indices associated with the presence of extremely high air temperatures were examined. Indices associated with heat waves, such as the number of hot days (T max ≥30°C) in the summer months (June, July, August) and beyond the summer months (May, September), the number of extremely hot days (T max ≥35°C), the duration of the longest hot spell in the year, as well as the number of tropical nights (T min ≤20°C) were calculated. Spatial distribution of change rate in days per decade for the studied indices as well as the significance level of the observed trends is illustrated. Also current values of the studied indices (for 1991-2013) are examined and compared with the reference period, . For eight of 11 analysed indexes, increase has been detected in last decades with the help of the Mann-Kendall test at a significance level ≥0.05 or better, for a large group of stations. Statistically significant increases of the number of hot days in summer, the number of tropical nights in a year, and duration of the longest hot spell in summer were found for more than half of the stations. Distinct changes in the duration of heat waves were also noted. In 1961-1990, the longest hot spell lasted for 10 days while in 1991-2013, there were many hot spells longer than that, while the longest hot spell recorded in this period lasted for 17 days. Beyond summer, changes in the number of hot days were smaller. In May, a statistically significant increase was recorded for only three stations, while in September the downward trend was dominating and for eight stations it was statistically significant.

show abstract

Section: Discussionsupporting

confidence: 90%

The heat goes on—changes in indices of hot extremes in Poland

Graczyk

Pińskwar

Kundzewicz

et al. 2016

Theor Appl Climatol

View full text Add to dashboard Cite

show abstract

“…Data quality control and assessment detected whether the recorded data were consistent with actual precipitation values (i.e., above 0 mm) and whether the daily maximum temperature exceeded the minimum temperature. In addition, the potential outliers based on the threshold, which is defined as the mean plus/minus 5 times the standard deviation, for daily temperature must be manually validated and corrected (Croitoru and Piticar, 2012).…”

Section: Datamentioning

confidence: 99%

Recent changes in extreme precipitation and drought over the Songhua River Basin, China, during 1960–2013

Song

Sun

et al. 2015

Atmospheric Research

159

View full text Add to dashboard Cite

Based on ten indices of extreme precipitation and one drought index (composite index, CI), the trends in extreme events were investigated using a Mann-Kendall non-parametric method at 39 stations in the Songhua River Basin (SHB) during 1960-2013. The regionally averaged wet-day precipitation (PRCPTOT) increased at a rate of 1.65 mm/year (R 2 = 0.28, P = 0.13), in which 82% of the stations experienced increases, but only 4 stations showed significant positive trends. The annual R95 and R99 exhibited slight upward trends at rates of 1.37 (R 2 = 0.21, P = 0.27) and 1.28 mm/year (R 2 = 0.23, P = 0.23) over the last 54 years; however, there were not significant trends in R95 and R99 at the 0.05 level. PRCPTOT, R95 and R99 showed similar spatial trends, in which positive trends mainly occurred in the northern and southeastern basins. The trends in the maximum 1-day precipitation (RX1day) and maximum 5-day precipitation (RX5day) do not show a prevalent trend (approximately 50% of the stations have a positive trend and the remaining stations have a negative trend). The simple daily intensity index (SDII) significantly decreased at an annual rate of 0.02 mm/d during 1960-2013 (R 2 = 0.66, P b 0.01); spatially, 49% of the stations experienced statistically significant decreases at the 0.05 level based on the Mann-Kendall non-parametric test. The regionally averaged heavy (R10mm) and very heavy precipitation days (R20mm) and consecutive wet days (CWD) showed no significant trends during the past 54 years; however, several individual extreme precipitation events, such as the flood of 1998 in the SHB, were well detected by these indices. The regionally averaged consecutive dry days (CDD) significantly increased (R 2 = 0.79, P b 0.01) at a rate of 0.22 days/year from 1960 to 2013. All of the stations exhibited statistically significant increases in CDD, excluding the Tongyu station in the western basin. The monthly RX5day values were highest in summer, from June to August, in the SHB; a peak occurred in July (67.5 mm) in the SHB during 1960-2013. The CI peaked in July, with the highest value of 0.2 in the SHB during 1960-2013. However, the two lowest CI values occurred in spring and fall, with values of −0.56 and −0.41, respectively. During April and May, when most of the spring drought events occur, a prevalent trend does not exist; moreover, almost no stations have statistically significant CI increases. In August and September, respectively 79% and 97% of the stations exhibited a CI negative trend, but only 2 and 6 stations showed significant decreases at the 0.05 level. The increasing extreme climate events present a challenge for local water resources management.

show abstract

“…Climate of Romania is on a significant warming and predominant drying, with an increasing frequency of warm and dry extremes, particularly in the southern and southeastern regions (Busuioc et al, 2010;Croitoru and Piticar, 2013;Birsan and Dumitrescu 2014;Busuioc et al, 2014;Bojariu et al 2015), also recognized as the most important agricultural regions of the country. These changes became visible from observational data since mid-to-late 1980s .…”

Section: Study-area In Romania and Context For Climate Adaptation Of mentioning

confidence: 99%

A farmer-based analysis of climate change adaptation options of agriculture in the Bărăgan Plain, Romania

et al. 2015

View full text Add to dashboard Cite

The paper has in view the assessment of the impact of climate change on agriculture in the main agricultural region of Romania (Bărăgan Plain), by understanding the contextual socio-economic factors of agriculture in the area as a key step towards climate adaptation, but also through identifying the user needs, awareness and requirements in terms of climate information. A special attention was given to the analysis of the changes in the socio-economic and political context of Romania since 1989, the post-communist period, marked by fundamental transformations in agriculture, with collective and state property being replaced by private property. The poor development of the productive services in agriculture resulted in the degradation of land's productive potential and the intensification the adverse effects of extreme climatic phenomena, proving a strong dependency of crop yields and productivity on climate. The mid-term (2021-2050) and long-term (2071-2100) climate variability and change of some key variables affecting crop development (air temperature, precipitation, evapotranspiration), under different scenarios have been investigated in relation to the potential impacts on main crops. A set of relevant climate extreme and agro-meteorological indices was further used to estimate the potential climate change impacts on agriculture. The study was focused on the interaction with farmers, the main actors of the climate adaptation process in the area, aiming to evaluate their perception and response to climate change. The research approach was mainly done through face-to-face interviews, as farmers did not respond positively to organised meetings. An important difference was noticed in terms of adaptive capacity between the large farms with a high adaptive capacity and low subsistence farms (family-run farms), the most vulnerable category to both socio-economic and climate change. The main climate adaptation measure considered crucial by the farmers is the rehabilitation/construction of irrigation systems. The study provides useful scientific insights which could improve the understanding of farmers and decision-makers on the potential impacts of the future climate change on crops, but also to mainstream climate adaptation actions in the agriculture policy.

show abstract

Changes in daily extreme temperatures in the extra‐Carpathians regions of Romania

Cited by 72 publications

References 52 publications

The heat goes on—changes in indices of hot extremes in Poland

The heat goes on—changes in indices of hot extremes in Poland

Recent changes in extreme precipitation and drought over the Songhua River Basin, China, during 1960–2013

A farmer-based analysis of climate change adaptation options of agriculture in the Bărăgan Plain, Romania

Contact Info

Product

Resources

About