Hristo Chervenkov

Dr. Hristo Chervenkov

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Research Focus & Metrics

Academic Career Length

21Years (2006-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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19 July 2012 in Climate Research
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Journal Article
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KJKatarzyna Juda-Rezler
Katarzyna Juda-Rezler
Magdalena ReizerMagdalena Reizer
Magdalena Reizer
PHPeter Huszar
Peter Huszar
BKBernd C. Krüger
Bernd C. Krüger
Prodromos ZanisProdromos Zanis
Prodromos Zanis
THTomas Halenka
Tomas Halenka

1 December 2011 in Climate Research
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Journal Article
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PHPeter Huszar
Peter Huszar
KJKatarzyna Juda-Rezler
Katarzyna Juda-Rezler
THT. Halenka
T. Halenka
HCHristo Chervenkov
Hristo Chervenkov
DSD. Syrakov
D. Syrakov
MBM. Belda
M. Belda

8 August 2020
Verified
Book Chapter
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HCHristo Chervenkov
Hristo Chervenkov
KSKiril Slavov
Kiril Slavov

18 January 2019
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Book Chapter
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HCHristo Chervenkov
Hristo Chervenkov
KSKiril Slavov
Kiril Slavov
VIVladimir Ivanov
Vladimir Ivanov

27 July 2022 in Atmosphere
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KMKrastina Doncheva Malcheva
Krastina Doncheva Malcheva
LBLilia Bocheva
Lilia Bocheva
HCHristo Chervenkov
Hristo Chervenkov
Many studies in the last few years have been dedicated to the increasing temperatures and extreme heat in Europe since the second half of the 20th century because of their adverse effects on ecosystems resilience, human health, and quality of life. The present research aims to analyze the spatio-temporal variations of extreme heat events in Southeastern Europe using daily temperature data from 70 selected meteorological stations and applying methodology developed initially for the quantitative assessment of hot weather in Bulgaria. We demonstrate the suitability of indicators based on maximum temperature thresholds to assess the intensity (i.e., magnitude and duration) and the tendency of extreme heat events in the period 1961–2020 both by individual stations and the Köppen’s climate zones. The capability of the used intensity-duration hot spell model to evaluate the severity of extreme heat events has also been studied and compared with the Excess Heat Factor severity index on a yearly basis. The study provides strong evidence of the suitability of the applied combined approach in the investigation of the spatio-temporal evolution of the hot weather phenomena over the considered domain.

4 April 2022 in Atmosphere
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HCHristo Chervenkov
Hristo Chervenkov
KSKiril Slavov
Kiril Slavov
The present study evaluates the National Aeronautics Space Administration (NASA) Earth Exchange Global Daily Downscaled Projections (NEX-GDDP) dataset that provides statistically downscaled CMIP5 historical and future climate projections of the daily precipitation sum and extreme temperatures at high spatial resolution. A multimodel ensemble from all 21 available models is composed and compared against gridded observations from E-OBS. The study is performed over Southeast Europe for the whole time span of the historical period of NEX-GDDP 1950–2005. The performance of the NEX-GDDP data was evaluated at multiple time scales such as annual, seasonal, monthly, and daily. The skill of the multimodel ensemble to reproduce the interannual variability, as well as the long-term trend, is also evaluated. Moreover, key climate indices of the Expert Team on Climate Change Detection and Indices (ETCCDI), derived from the ensemble extreme temperatures and precipitation are superimposed on their counterparts based on the reference dataset E-OBS. Findings of the performed research indicate that NEX-GDDP parameters are in good agreement with the reference over the considered period on monthly, seasonal and annual scales which agrees with the outcomes from similar studies for other parts of the world. There are also no systematic differences in the pattern of the biases of the minimum and maximum temperature. Generally, the multimodel ensemble reproduces the extreme temperatures significantly better than the precipitation sum. The analysis reveals also the nonnegligible inefficiency of the NEX-GDDP ensemble to reproduce the long-term trend of the considered parameters as well as the climate extremes expressed with the ETCCDI indices.